华北克拉通北缘张家口-宣化地区古生代-中生代岩浆构造活动与成矿作用

甄世民, 王大钊, 白海军, 贾儒雅, 王江, 查钟健, 李阳, 缪建普. 2021. 华北克拉通北缘张家口-宣化地区古生代-中生代岩浆构造活动与成矿作用. 岩石学报, 37(6): 1619-1652. doi: 10.18654/1000-0569/2021.06.01
引用本文: 甄世民, 王大钊, 白海军, 贾儒雅, 王江, 查钟健, 李阳, 缪建普. 2021. 华北克拉通北缘张家口-宣化地区古生代-中生代岩浆构造活动与成矿作用. 岩石学报, 37(6): 1619-1652. doi: 10.18654/1000-0569/2021.06.01
ZHEN ShiMin, WANG DaZhao, BAI HaiJun, JIA RuYa, WANG Jiang, ZHA ZhongJian, LI Yang, MIAO JianPu. 2021. The Paleozoic-Mesozoic magmatic-tectonic activities and their geological implications in the Zhangjiakou-Xuanhua district, northern margin of the North China Craton. Acta Petrologica Sinica, 37(6): 1619-1652. doi: 10.18654/1000-0569/2021.06.01
Citation: ZHEN ShiMin, WANG DaZhao, BAI HaiJun, JIA RuYa, WANG Jiang, ZHA ZhongJian, LI Yang, MIAO JianPu. 2021. The Paleozoic-Mesozoic magmatic-tectonic activities and their geological implications in the Zhangjiakou-Xuanhua district, northern margin of the North China Craton. Acta Petrologica Sinica, 37(6): 1619-1652. doi: 10.18654/1000-0569/2021.06.01

华北克拉通北缘张家口-宣化地区古生代-中生代岩浆构造活动与成矿作用

  • 基金项目:

    本文受中国地质调查局地质矿产调查专项(DD20190159、DD20160052、DD20190166)和国家自然科学基金项目(9260019、42003032、41573036)联合资助

详细信息
    作者简介:

    甄世民, 男, 1984年生, 博士, 高级工程师, 主要从事矿床学研究, E-mail: zhenshimin0001@163.com

    通讯作者: 王大钊, 男, 1991年生, 讲师, 主要从事矿床学研究, E-mail: wangdazhao@ecut.edu.cn
  • 中图分类号: P588.1;P597.3;P618.51

The Paleozoic-Mesozoic magmatic-tectonic activities and their geological implications in the Zhangjiakou-Xuanhua district, northern margin of the North China Craton

More Information
  • 河北省张家口-宣化地区(张宣地区)位于华北克拉通北缘中段,区内自显生宙以来构造活动频繁,并产出大量岩浆岩和金矿床,是研究华北克拉通北缘岩浆-构造-成矿演化体系的重要对象。本文通过对张宣地区的水泉沟正长岩、响水沟似斑状花岗岩、井儿洼粗安岩-英安岩、象山花岗闪长岩、青羊沟黑云母二长花岗岩和张家口组流纹岩的锆石年龄、Lu-Hf同位素和地球化学组成进行研究,结合前人研究成果,获得区内古生代-中生代岩浆岩的侵位时期主要为海西期(峰值398Ma和373Ma)、印支期(峰值234Ma)和燕山期(峰值143Ma和130Ma)。张宣地区在古生代-中生代经历了古亚洲洋俯冲、华北克拉通破坏及古太平洋俯冲过程。早古生代时期,古亚洲洋向华北克拉通俯冲;到泥盆纪,白乃庙岛弧带和华北克拉通北缘发生弧陆碰撞,张宣地区处于弧陆碰撞后的伸展环境,富集地幔岩浆上涌并经历了地壳的同化混染和分离结晶的共同作用,形成大量碱性岩;二叠纪末期-三叠纪,各微陆块相互碰撞,张宣地区处于碰撞后伸展阶段,地幔岩浆引起加厚下地壳的部分熔融,基性、酸性岩浆混合,导致区内的基性岩与酸性岩共存;侏罗纪-白垩纪时期,华北克拉通发生减薄,形成区内大范围的侵入岩和火山岩。张宣地区产有大量金矿、铅锌矿、银矿及少量铜矿和钼矿,金矿集中产于宣化-崇礼-赤城交界处,而银铅锌多金属矿则成群成带环绕金矿化集中区分布。成矿时间主要为海西期和燕山期,印支期成矿尚未明确,但成矿潜力巨大。根据地质特征和同位素组成,可将张宣地区的金矿床划分为"东坪式"、"小营盘式"和"张全庄式"三类。古生代-中生代各时期岩浆活动对金成矿均有贡献,大部分金矿床与海西期和燕山期岩浆活动联系密切,多期次成矿及成矿叠加是形成张宣地区大量金矿床的重要因素。

  • 加载中
  • 图 1 

    张宣地区大地构造位置(a)及区域地质简图(b)(据甄世民等, 2019)

    Figure 1. 

    Sketch maps of (a) geotectonic location and (b) tectonic-magmatic framework of the Zhangjiakou-Xuanhua area

    图 2 

    张宣地区地质矿产图(据Zhen et al., 2020)

    Figure 2. 

    Sketch map of geology and ore deposits of the Zhangjiakou-Xuanhua area (modified after Zhen et al., 2020)

    图 3 

    张宣地区岩浆岩野外及镜下照片

    Figure 3. 

    Field photos and microphotographs of magmatic rocks in the Zhangjiakou-Xuanhua area

    图 4 

    张宣地区古生代-中生代岩浆岩锆石CL图像

    Figure 4. 

    Zircon CL images of the Paleozoic-Mesozoic igneous rocks from the Zhangjiakou-Xuanhua area

    图 5 

    张宣地区古生代-中生代岩浆岩锆石U-Pb年龄

    Figure 5. 

    Zircon U-Pb ages of the PaleozoicMesozoic igneous rocks from the Zhangjiakou-Xuanhua area

    图 6 

    张宣地区古生代-中生代岩浆岩球粒陨石标准化稀土元素配分图和原始地幔标准化微量元素蛛网图(标准化值据Sun and McDonough, 1989)

    Figure 6. 

    Chondrite-normalized REE patterns and primitive mantle-normalized element spider diagrams for the Paleozoic-Mesozoic igneous rocks from the Zhangjiakou-Xuanhua area (normalization values after Sun and McDonough, 1989)

    图 7 

    张宣地区古生代-中生代岩浆岩成岩年龄统计图

    Figure 7. 

    Statistical diagram of diagenetic ages for the PaleozoicMesozoic igneous rocks from the Zhangjiakou-Xuanhua area

    图 8 

    张宣地区古生代-中生代岩浆岩Hf同位素分布图

    Figure 8. 

    Scattergrams of Hf isotope compositions for the Paleozoic-Mesozoic igneous rocks from the Zhangjiakou-Xuanhua area

    图 9 

    张宣地区古生代-中生代岩浆岩Sr-Nd同位素分布图

    Figure 9. 

    Scattergrams of Sr-Nd isotope compositions for the Paleozoic-Mesozoic igneous rocks from the Zhangjiakou-Xuanhua area

    图 10 

    水泉沟碱性杂岩体哈克图解

    Figure 10. 

    Harker diagrams of the Shuiquangou alkaline complex

    图 11 

    张宣地区三叠纪花岗岩埃达克岩判别图解(底图据Defant and Drummond, 1993)

    Figure 11. 

    Discrimination diagrams of adakitic rocks for the Triassic granites from the Zhangjiakou-Xuanhua area (base map after Defant and Drummond, 1993)

    图 12 

    张宣地区晚侏罗世-早白垩世岩浆岩A型花岗岩和高分异花岗岩判别图解(底图据Whalen et al., 1987)

    Figure 12. 

    Discrimination diagrams of A-type and highly-fractionated granites for the Late Jurassic-Early Cretaceous igneous rocks from the Zhangjiakou-Xuanhua area (base map after Whalen et al., 1987)

    图 13 

    张宣地区古生代-中生代岩浆-构造演化模式图

    Figure 13. 

    Model of the Paleozoic-Mesozoic magmatic-tectonic evolution from the Zhangjiakou-Xuanhua area

    图 14 

    张宣地区金矿床H-O-S-Pb-He-Ar同位素组成(a, 底图据Taylor, 1974; c, d, 底图据Zartman and Doe, 1981;e, f, 底图据Mamyrin and Tolstikhin, 1984)

    Figure 14. 

    H-O-S-Pb-He-Ar isotope compositions of gold deposits in the Zhangjiakou-Xuanhua area (a, after Taylor, 1974; c, d, after Zartman and Doe, 1981; e, f, after Mamyrin and Tolstikhin, 1984)

    图 15 

    张宣地区成岩成矿年龄分布图

    Figure 15. 

    Distribution diagram of diagenetic and metallogenic ages from the Zhangjiakou-Xuanhua area

    表 1 

    张宣地区岩浆岩锆石U-Pb年龄

    Table 1. 

    Zircon U-Pb ages of igneous rocks from the Zhangjiakou-Xuanhua area

    测点号 Th/U 同位素比值 年龄(Ma)
    1σ 1σ 1σ 1σ 1σ 1σ
    SQG-1水泉沟正长岩
    -1 19 85 0.22 0.0598 0.0028 0.5142 0.0240 0.0639 0.0008 570 104 422 16 399 5
    -2 68 238 0.28 0.0561 0.0017 0.4837 0.0151 0.0634 0.0006 440 74 402 10 396 3
    -3 7 45 0.15 0.0551 0.0036 0.4560 0.0255 0.0633 0.0012 389 152 382 18 396 7
    -4 4 28 0.15 0.0670 0.0049 0.5669 0.0377 0.0637 0.0012 818 150 457 25 399 7
    -5 41 329 0.12 0.0569 0.0014 0.4963 0.0112 0.0643 0.0006 461 56 410 8 402 4
    -6 2 19 0.11 0.0518 0.0051 0.4489 0.0363 0.0637 0.0014 246 218 377 26 399 8
    -7 14 72 0.19 0.0556 0.0027 0.4770 0.0228 0.0637 0.0008 474 106 397 16 398 5
    -8 3 29 0.10 0.0513 0.0039 0.4349 0.0318 0.0637 0.0014 224 180 368 23 398 8
    -9 31 256 0.12 0.0567 0.0016 0.4933 0.0141 0.0637 0.0006 462 62 408 10 398 4
    -10 6 52 0.12 0.0501 0.0029 0.4359 0.0244 0.0630 0.0008 167 133 368 17 394 5
    -11 2 14 0.11 0.0646 0.0064 0.5353 0.0426 0.0639 0.0017 742 212 437 28 399 10
    -12 45 236 0.19 0.0559 0.0017 0.4748 0.0143 0.0628 0.0008 423 70 395 10 393 5
    -13 2 20 0.11 0.0606 0.0064 0.4693 0.0377 0.0616 0.0013 600 233 392 26 385 8
    -14 32 217 0.15 0.0560 0.0016 0.4858 0.0145 0.0639 0.0007 423 68 403 10 399 4
    -15 35 151 0.23 0.0573 0.0020 0.4944 0.0171 0.0636 0.0007 485 79 409 12 398 4
    -16 16 61 0.26 0.0590 0.0031 0.5017 0.0248 0.0634 0.0009 609 121 414 17 396 5
    -17 641 1856 0.35 0.0550 0.0010 0.4875 0.0089 0.0650 0.0006 382 37 404 6 406 4
    -18 3 19 0.15 0.0776 0.0097 0.6395 0.0646 0.0639 0.0018 1123 258 504 40 399 11
    -19 279 595 0.47 0.0601 0.0017 0.5311 0.0145 0.0648 0.0007 585 57 434 10 405 5
    -20 28 366 0.08 0.0542 0.0014 0.4783 0.0122 0.0649 0.0008 352 62 398 9 406 5
    -21 2541 2715 0.94 0.0550 0.0009 0.4904 0.0089 0.0653 0.0008 395 38 406 6 408 5
    -22 15 91 0.17 0.0563 0.0028 0.4844 0.0226 0.0638 0.0011 438 144 402 16 399 7
    -23 11 54 0.20 0.0537 0.0030 0.4647 0.0246 0.0646 0.0011 329 134 388 17 404 7
    -24 20 108 0.18 0.0569 0.0028 0.4942 0.0222 0.0643 0.0009 461 113 409 15 402 6
    -25 26 104 0.25 0.0658 0.0028 0.5670 0.0259 0.0634 0.0015 780 90 457 17 396 9
    -26 676 1657 0.41 0.0543 0.0011 0.4783 0.0100 0.0647 0.0007 355 49 398 7 404 4
    -27 92 365 0.25 0.0569 0.0014 0.4979 0.0123 0.0643 0.0006 461 56 411 8 402 4
    -28 45 623 0.07 0.0560 0.0014 0.4926 0.0141 0.0644 0.0009 427 56 408 10 402 6
    XSG-5响水沟似斑状花岗岩
    -1 295 430 0.69 0.0528 0.0026 0.2628 0.0129 0.0360 0.0005 317 115 237 10 228 3
    -2 204 386 0.53 0.0547 0.0026 0.2726 0.0127 0.0360 0.0005 398 101 245 10 228 3
    -3 169 390 0.43 0.0525 0.0028 0.2682 0.0145 0.0371 0.0005 309 119 241 12 235 3
    -4 111 218 0.51 0.0632 0.0037 0.3256 0.0200 0.0369 0.0006 722 126 286 15 234 4
    -5 167 339 0.49 0.0534 0.0027 0.2759 0.0149 0.0370 0.0005 346 115 247 12 235 3
    -6 640 471 1.36 0.0519 0.0026 0.2666 0.0132 0.0370 0.0005 283 117 240 11 234 3
    -7 108 252 0.43 0.0559 0.0049 0.2762 0.0237 0.0360 0.0009 456 196 248 19 228 6
    -8 81 104 0.77 0.1155 0.0093 0.2880 0.0252 0.0189 0.0005 1888 114 257 20 120 3
    -9 121 175 0.69 0.0638 0.0052 0.3109 0.0237 0.0360 0.0006 744 174 275 18 228 4
    -10 233 334 0.70 0.0589 0.0037 0.3066 0.0197 0.0373 0.0006 565 137 272 15 236 4
    -11 240 353 0.68 0.0544 0.0044 0.2777 0.0200 0.0374 0.0007 387 183 249 16 237 4
    -12 90 100 0.90 0.0635 0.0053 0.3005 0.0249 0.0355 0.0009 724 181 267 19 225 6
    -13 405 514 0.79 0.0517 0.0024 0.2637 0.0125 0.0365 0.0004 333 105 238 10 231 3
    -14 83 213 0.39 0.0599 0.0037 0.3088 0.0177 0.0378 0.0006 598 131 273 14 239 4
    -15 214 431 0.50 0.0513 0.0023 0.2493 0.0111 0.0349 0.0004 254 104 226 9 221 3
    JEW-01井儿洼粗安岩-英安岩
    -1 55 77 0.72 0.0582 0.0151 0.2044 0.0537 0.0259 0.0015 539 494 189 45 165 10
    -2 41 96 0.43 0.0723 0.0237 0.1784 0.0384 0.0247 0.0014 994 710 167 33 158 8
    -3 250 309 0.81 0.0526 0.0057 0.1881 0.0151 0.0272 0.0008 309 248 175 13 173 5
    -4 25 45 0.55 0.0568 0.0202 0.1674 0.0489 0.0245 0.0015 483 637 157 43 156 10
    -5 206 341 0.60 0.0523 0.0059 0.1813 0.0146 0.0259 0.0008 298 292 169 13 165 5
    -6 60 83 0.72 0.0526 0.0114 0.2002 0.0313 0.0278 0.0012 309 431 185 26 177 7
    -7 99 120 0.83 0.0682 0.0177 0.1860 0.0424 0.0258 0.0011 876 558 173 36 164 7
    -8 111 164 0.68 0.0800 0.0184 0.1928 0.0318 0.0242 0.0011 1198 469 179 27 154 7
    T-PM00-1象山花岗闪长岩
    -1 81 100 0.81 0.0586 0.0052 0.1576 0.0123 0.0201 0.0004 550 201 149 11 128 3
    -2 118 122 0.96 0.0588 0.0062 0.1542 0.0150 0.0203 0.0004 567 232 146 13 129 3
    -3 84 90 0.94 0.0560 0.0056 0.1525 0.0136 0.0210 0.0006 454 222 144 12 134 4
    -4 227 184 1.23 0.0642 0.0051 0.1912 0.0155 0.0215 0.0005 746 167 178 13 137 3
    -5 180 186 0.97 0.0550 0.0038 0.1631 0.0101 0.0221 0.0004 409 153 153 9 141 2
    -6 303 231 1.31 0.1269 0.0093 0.4297 0.0348 0.0231 0.0004 2055 130 363 25 147 3
    -7 75 98 0.77 0.0537 0.0051 0.1573 0.0123 0.0220 0.0005 367 219 148 11 140 3
    -8 150 202 0.74 0.0495 0.0034 0.1468 0.0087 0.0217 0.0004 172 159 139 8 138 2
    -9 123 108 1.13 0.1941 0.0126 0.6754 0.0479 0.0246 0.0007 2777 73 524 29 157 4
    -10 70 94 0.74 0.0971 0.0482 0.3237 0.2098 0.0212 0.0005 1569 1076 285 161 135 3
    -11 105 154 0.68 0.0529 0.0035 0.1468 0.0084 0.0210 0.0004 324 156 139 7 134 3
    -12 56 69 0.81 0.0536 0.0063 0.1509 0.0150 0.0211 0.0006 354 268 143 13 135 4
    -14 72 93 0.78 0.0613 0.0058 0.1707 0.0130 0.0215 0.0005 650 204 160 11 137 3
    -15 106 142 0.75 0.0974 0.0420 0.3205 0.1562 0.0237 0.0005 1576 894 282 120 151 3
    -16 405 287 1.41 0.0489 0.0027 0.1360 0.0070 0.0201 0.0003 146 162 130 6 128 2
    -17 139 129 1.08 0.0440 0.0052 0.1414 0.0202 0.0226 0.0005 - - 134 18 144 3
    -18 126 154 0.81 0.0561 0.0038 0.1636 0.0107 0.0214 0.0004 454 150 154 9 137 3
    -19 100 126 0.79 0.0560 0.0045 0.1605 0.0115 0.0210 0.0004 454 184 151 10 134 3
    -20 140 148 0.94 0.0516 0.0041 0.1507 0.0101 0.0214 0.0004 333 185 143 9 137 3
    -21 134 145 0.92 0.0511 0.0043 0.1475 0.0113 0.0210 0.0004 256 198 140 10 134 3
    -22 113 145 0.78 0.1217 0.0108 0.4382 0.0397 0.0242 0.0006 1983 158 369 28 154 4
    -23 104 109 0.95 0.0525 0.0047 0.1502 0.0112 0.0216 0.0004 306 206 142 10 138 3
    -24 59 73 0.81 0.0530 0.0070 0.1554 0.0149 0.0233 0.0006 328 278 147 13 149 4
    -25 146 177 0.82 0.0652 0.0070 0.2047 0.0225 0.0235 0.0004 783 197 189 19 150 3
    -26 341 225 1.52 0.0584 0.0039 0.1806 0.0107 0.0228 0.0003 546 145 169 9 145 2
    -27 122 152 0.80 0.0484 0.0041 0.1466 0.0101 0.0227 0.0005 120 185 139 9 145 3
    -29 56 71 0.79 0.0570 0.0064 0.1658 0.0156 0.0224 0.0006 500 250 156 14 143 4
    -30 72 95 0.76 0.0587 0.0061 0.1700 0.0160 0.0221 0.0009 567 223 159 14 141 6
    -32 144 182 0.79 0.0607 0.0051 0.1783 0.0154 0.0216 0.0004 628 182 167 13 137 3
    -33 133 152 0.88 0.0511 0.0053 0.1643 0.0143 0.0250 0.0006 256 217 154 12 159 4
    -34 192 197 0.97 0.0511 0.0037 0.1547 0.0102 0.0219 0.0004 256 170 146 9 140 2
    -35 103 103 1.00 0.0566 0.0055 0.1581 0.0133 0.0209 0.0004 476 212 149 12 133 3
    B0169青羊沟黑云母二长花岗岩
    -1 404 192 2.10 0.0503 0.0019 0.1402 0.0051 0.0205 0.0002 206 89 133 5 131 2
    -2 1100 569 1.93 0.0739 0.0045 0.2105 0.0147 0.0201 0.0002 1039 128 194 12 128 1
    -3 311 237 1.31 0.0480 0.0020 0.1320 0.0053 0.0201 0.0002 102 -103 126 5 128 1
    -4 392 349 1.12 0.1149 0.0074 0.3631 0.0256 0.0217 0.0003 1880 117 315 19 138 2
    -5 602 379 1.59 0.0856 0.0054 0.2551 0.0177 0.0209 0.0003 1329 90 231 14 133 2
    -6 552 176 3.13 0.0479 0.0024 0.1254 0.0066 0.0190 0.0002 98 115 120 6 121 1
    -7 64 51 1.26 0.0561 0.0038 0.1780 0.0114 0.0232 0.0004 457 150 166 10 148 3
    -8 490 241 2.04 0.0500 0.0018 0.1328 0.0047 0.0193 0.0002 198 85 127 4 123 1
    -9 412 183 2.24 0.0467 0.0021 0.1283 0.0057 0.0201 0.0002 32 107 123 5 128 1
    -10 706 371 1.90 0.0581 0.0028 0.1811 0.0116 0.0217 0.0003 600 101 169 10 138 2
    -11 673 430 1.57 0.0502 0.0015 0.1392 0.0038 0.0201 0.0002 211 67 132 3 128 1
    -12 1135 647 1.75 0.0551 0.0012 0.1530 0.0036 0.0201 0.0002 417 50 145 3 128 1
    -13 475 304 1.56 0.0529 0.0021 0.1632 0.0071 0.0223 0.0003 324 91 153 6 142 2
    -14 222 174 1.27 0.1858 0.0107 0.6734 0.0500 0.0238 0.0005 2705 95 523 30 152 3
    -15 253 181 1.40 0.0459 0.0022 0.1242 0.0059 0.0197 0.0003 error 119 5 126 2
    -16 363 207 1.75 0.0549 0.0028 0.1643 0.0085 0.0217 0.0003 409 108 154 7 138 2
    -17 170 172 0.99 0.0553 0.0030 0.1602 0.0084 0.0212 0.0003 433 120 151 7 135 2
    -18 60 46 1.30 0.0537 0.0054 0.1447 0.0124 0.0201 0.0005 367 223 137 11 128 3
    -19 1046 559 1.87 0.0471 0.0013 0.1408 0.0040 0.0216 0.0002 54 63 134 4 138 1
    -20 1316 603 2.18 0.0501 0.0014 0.1395 0.0041 0.0201 0.0002 211 32 133 4 128 1
    ZJK-1张家口组流纹岩
    -1 51 44 1.17 0.0513 0.0064 0.1434 0.013 0.0214 0.0005 254 263 136 11.6 136 3.4
    -2 54 47 1.15 0.0556 0.0069 0.1582 0.0148 0.0224 0.0007 435 284 149 13 143 4.3
    -3 71 56 1.27 0.0515 0.0061 0.1481 0.0139 0.0214 0.0005 265 252 140 12.3 136 3.1
    -4 46 40 1.16 0.0543 0.007 0.1464 0.014 0.0213 0.0006 389 297 139 12.4 136 3.5
    -5 101 52 1.95 0.0533 0.0099 0.1636 0.0228 0.0239 0.0012 343 380 154 19.9 152 7.3
    -6 49 49 1.01 0.0733 0.011 0.172 0.0164 0.0188 0.0007 1020 308 161 14.2 120 4.6
    -7 41 35 1.18 0.0589 0.0082 0.1654 0.0183 0.0217 0.0006 561 304 155 15.9 138 3.9
    -8 64 59 1.08 0.0742 0.0082 0.1933 0.0189 0.0198 0.0006 1048 226 179 16.1 126 3.5
    -9 39 34 1.15 0.0633 0.0118 0.1387 0.0104 0.0213 0.0007 720 404 132 9.3 136 4.5
    -10 103 62 1.66 0.0535 0.0055 0.1414 0.0115 0.0207 0.0005 350 235 134 10.2 132 3.3
    -11 75 58 1.29 0.0597 0.0059 0.1556 0.0113 0.0207 0.0005 591 215 147 9.9 132 3.1
    -12 49 41 1.18 0.0591 0.0082 0.1492 0.0118 0.0207 0.0006 569 310 141 10.4 132 3.7
    -13 186 105 1.77 0.0492 0.0043 0.138 0.0101 0.0214 0.0004 154 196 131 9 136 2.6
    -14 80 50 1.6 0.0497 0.0061 0.1311 0.0124 0.021 0.0005 189 267 125 11.1 134 3
    -15 44 37 1.19 0.0576 0.0084 0.1475 0.0143 0.0211 0.0005 522 319 140 12.6 134 3.4
    -16 47 42 1.12 0.1049 0.0124 0.2964 0.0318 0.0207 0.0006 1722 218 264 24.9 132 3.7
    -17 49 42 1.16 0.0558 0.0078 0.1474 0.0162 0.0212 0.0006 443 315 140 14.4 135 3.6
    -18 57 48 1.21 0.0463 0.0057 0.1299 0.0152 0.0209 0.0005 16.8 270 124 13.6 133 3.3
    -19 277 381 0.73 0.0514 0.0024 0.1501 0.0068 0.0214 0.0003 257 107 142 6 136 1.8
    -20 136 78 1.75 0.0534 0.0056 0.1452 0.0126 0.021 0.0005 343 239 138 11.2 134 2.9
    -21 82 53 1.54 0.0868 0.0074 0.2379 0.0157 0.0212 0.0005 1367 165 217 12.8 135 3.4
    下载: 导出CSV

    表 2 

    张宣地区岩浆岩锆石Lu-Hf同位素组成

    Table 2. 

    Zircon Lu-Hf isotope compositions of igneous rocks from the Zhangjiakou-Xuanhua area

    测点号 年龄(Ma) 176Yb/177Hf 1σ 176Lu/177Hf 1σ 176Hf/177Hf 1σ εHf(0) εHf(t) tDM (Ma) tDMC (Ma) fLu/Hf
    SQG-1水泉沟正长岩
    -1 399 0.006646 0.00004 0.000328 0.00000 0.281947 0.00002 -29.2 -20.5 1802 2682 -0.99
    -2 396 0.024322 0.00030 0.001156 0.00001 0.281946 0.00001 -29.2 -20.8 1844 2700 -0.97
    -6 399 0.003355 0.00009 0.000173 0.00001 0.281903 0.00001 -30.7 -22.0 1855 2778 -0.99
    -7 398 0.005230 0.00015 0.000272 0.00001 0.281970 0.00002 -28.4 -19.7 1768 2631 -0.99
    -16 396 0.019718 0.00018 0.000964 0.00001 0.281944 0.00002 -29.3 -20.9 1837 2702 -0.97
    -22 399 0.004203 0.00007 0.000221 0.00000 0.281915 0.00001 -30.3 -21.6 1841 2752 -0.99
    -23 404 0.006368 0.00012 0.000331 0.00001 0.281919 0.00002 -30.2 -21.4 1841 2741 -0.99
    -24 402 0.008293 0.00023 0.000423 0.00001 0.281879 0.00002 -31.6 -22.9 1900 2833 -0.99
    XSG-5响水沟似斑状花岗岩
    -1 228 0.013945 0.00004 0.000562 0.00000 0.282179 0.00001 -21.0 -16.1 1496 2278 -0.98
    -2 228 0.013978 0.00044 0.000544 0.00001 0.282161 0.00001 -21.6 -16.7 1518 2316 -0.98
    -3 235 0.017295 0.00039 0.000690 0.00001 0.282178 0.00001 -21.0 -15.9 1501 2275 -0.98
    -4 234 0.016069 0.00014 0.000664 0.00001 0.282172 0.00001 -21.2 -16.2 1509 2290 -0.98
    -8 228 0.015461 0.00021 0.000629 0.00001 0.282186 0.00001 -20.7 -15.8 1488 2262 -0.98
    -10 228 0.019892 0.00031 0.000759 0.00001 0.282142 0.00001 -22.3 -17.4 1554 2361 -0.98
    -14 225 0.039011 0.00033 0.001493 0.00001 0.282266 0.00001 -17.9 -13.2 1409 2092 -0.96
    -15 231 0.024712 0.00031 0.000938 0.00001 0.282163 0.00001 -21.5 -16.6 1532 2314 -0.97
    JEW-1井儿洼粗安岩-英安岩
    -1 165 0.027743 0.00045 0.001019 0.00001 0.282538 0.00005 -8.3 -4.8 1011 1516 -0.97
    -2 158 0.048221 0.00018 0.001797 0.00001 0.282607 0.00005 -5.8 -2.6 933 1372 -0.95
    -3 173 0.085136 0.00083 0.003179 0.00003 0.282855 0.00006 2.9 6.4 597 811 -0.90
    -5 165 0.034647 0.00019 0.001414 0.00001 0.282271 0.00003 -17.7 -14.2 1399 2116 -0.96
    -6 177 0.047679 0.00045 0.001664 0.00002 0.282776 0.00004 0.1 3.8 687 977 -0.95
    -7 164 0.031591 0.00030 0.001142 0.00001 0.282691 0.00006 -2.9 0.6 798 1173 -0.97
    -8 154 0.039777 0.00011 0.001437 0.00000 0.282567 0.00005 -7.2 -4.3 981 1467 -0.96
    T-PM00-1象山花岗闪长岩
    -4 137 0.023427 0.00021 0.000978 0.00001 0.281980 0.00002 -28.0 -25.1 1787 2776 -0.97
    -5 141 0.020044 0.00012 0.000887 0.00001 0.282035 0.00002 -26.1 -23.1 1708 2653 -0.97
    -8 138 0.026396 0.00014 0.001152 0.00001 0.282026 0.00002 -26.4 -23.5 1732 2675 -0.97
    -10 135 0.023608 0.00011 0.000989 0.00000 0.282033 0.00002 -26.1 -23.2 1715 2661 -0.97
    -14 137 0.007391 0.00005 0.000322 0.00000 0.282046 0.00002 -25.7 -22.7 1668 2628 -0.99
    -18 137 0.013641 0.00008 0.000618 0.00000 0.282064 0.00002 -25.0 -22.1 1655 2588 -0.98
    -20 137 0.190456 0.00031 0.000832 0.00001 0.282012 0.00002 -26.9 -24.0 1737 2706 -0.97
    -23 138 0.016664 0.00014 0.000712 0.00001 0.282090 0.00002 -24.1 -21.1 1623 2530 -0.98
    -30 141 0.014425 0.00005 0.000639 0.00000 0.282067 0.00002 -24.9 -21.9 1652 2579 -0.98
    -29 143 0.009203 0.00002 0.000418 0.00000 0.282051 0.00002 -25.5 -22.4 1664 2612 -0.99
    -32 137 0.015310 0.00003 0.000694 0.00000 0.282056 0.00002 -25.3 -22.4 1670 2607 -0.98
    -34 140 0.014320 0.00021 0.000636 0.00001 0.282036 0.00002 -26.0 -23.0 1695 2650 -0.98
    B-0169青羊沟黑云母二长花岗岩
    -01 131 0.044784 0.00011 0.001472 0.00001 0.282051 0.00002 -25.5 -22.8 1712 2627 -0.96
    -04 138 0.068482 0.00045 0.002140 0.00001 0.282122 0.00001 -23.0 -20.3 1641 2470 -0.94
    -06 121 0.049489 0.00023 0.001647 0.00001 0.282047 0.00002 -25.6 -22.9 1726 2636 -0.95
    -07 148 0.060908 0.00008 0.002003 0.00000 0.282063 0.00002 -25.1 -22.3 1719 2600 -0.94
    -09 128 0.068334 0.00046 0.002272 0.00001 0.282099 0.00002 -23.8 -21.1 1680 2522 -0.93
    ZJK-1张家口组流纹岩
    -3 136 0.024759 0.00022 0.000958 0.00001 0.282270 0.00001 -17.8 -14.9 1384 2133 -0.97
    -4 136 0.016421 0.00011 0.000643 0.00001 0.282309 0.00002 -16.4 -13.4 1318 2043 -0.98
    -9 136 0.019441 0.00020 0.000768 0.00001 0.282231 0.00001 -19.1 -16.2 1431 2218 -0.98
    -11 132 0.029273 0.00024 0.001107 0.00001 0.282242 0.00001 -18.7 -15.9 1429 2198 -0.97
    -13 136 0.067141 0.00060 0.002535 0.00002 0.282225 0.00002 -19.3 -16.6 1509 2241 -0.92
    -17 135 0.056560 0.00128 0.002176 0.00005 0.282259 0.00002 -18.1 -15.4 1446 2164 -0.93
    -20 134 0.015795 0.00016 0.000619 0.00001 0.282264 0.00001 -18.0 -15.1 1380 2146 -0.98
    下载: 导出CSV

    表 3 

    张宣地区岩浆岩全岩主量(wt%)、微量(×10-6)元素组成

    Table 3. 

    Whole-rock major (wt%) and trace (×10-6) element compositions of igneous rocks from the Zhangjiakou-Xuanhua area

    样品号 SQG-1 SQG-2 SQG-3 XSG-2 XSG-3 XSG-4 XSG-5 T-PM00-38 T-PM00-39 T-PM00-40 T-PM00-41 T-PM00-42 T-PM00-43
    岩性 水泉沟正长岩 响水沟似斑状花岗岩 象山花岗闪长岩
    SiO2 63.79 63.6 64.79 71.06 71.04 68.45 61.36 68.9 67.86 67.19 71.18 69.26 69.15
    TiO2 0.16 0.11 0.12 0.16 0.18 0.18 0.2 0.64 0.79 0.77 0.61 0.63 0.73
    Al2O3 19.02 18.8 18.92 15.94 15.94 16.22 20.21 12.5 11.83 12.52 12.06 12.24 12.12
    Fe2O3T 1.37 1.34 1.31 1.07 1.12 0.93 1.37 4.51 5.57 5.65 4.1 4.66 4.81
    MnO 0.04 0.05 0.08 0.02 0.02 0.03 0.03 0.1 0.12 0.15 0.11 0.14 0.11
    MgO 0.12 0.08 0.06 0.26 0.29 0.26 0.33 3.65 3.63 3.72 2.48 3.6 3.72
    CaO 1.66 1.61 1.82 1.55 1.6 2.34 2.01 0.57 0.63 0.66 0.49 0.59 0.61
    Na2O 6.43 6 7.23 5.08 5.08 3.26 6.89 1.43 1.26 1.49 1.41 1.44 1.44
    K2O 5.57 6.49 4.98 3.44 3.34 3.47 3.81 6.26 7.18 6.25 6.06 5.82 6.19
    P2O5 0.01 0.02 0.01 0.05 0.05 0.06 0.05 0.15 0.14 0.2 0.15 0.16 0.21
    Total 99.4 99.31 100.5 99.59 99.67 96.04 97.49 99.58 99.52 99.52 99.69 99.62 99.56
    Mg# 17 12 10 36 38 39 36 65 60 61 58 64 64
    Li 2.9 2.7 1.7 18.8 12.9 23.7 9.8 13.3 20.3 19.6 15.4 18.7 21.1
    Be 1.23 1.31 1.09 2.65 2.25 1.73 6.03 1.82 2.12 1.95 2.14 2.04 1.75
    Sc 1.6 1.1 0.9 1.9 2.3 2.2 3.8 3.7 3.6 4.2 3.2 4.1 3.6
    V 30 34 32 11 10 10 14 31 37 38 28 32 33
    Cr 4 2 - 8 9 13 10 1 10 1 6 13 6
    Co 1.3 0.9 0.4 1.2 1.2 1.4 1.5 5.4 6.5 5.6 4.7 5.7 6
    Ni 1.5 0.4 .- 0.5 0.6 0.5 0.4 2.1 4.7 1.9 3.7 8.7 4.2
    Cu 0.7 7.5 1.9 1.2 0.5 .- 0.7 3.4 2.5 4.9 6.3 3.8 2.3
    Zn 33 19 17 38 44 37 44 70 45 62 53 61 47
    Ga 21.1 19.75 20.4 22.5 20.8 20.2 33.2 18.5 18.5 19.1 17.7 19.5 18.9
    Rb 75.7 88.9 64.5 101.5 90.3 96.4 136.5 143.3 159.5 126.3 131.3 131.9 127.9
    Sr 2550 1740 907 915 850 576 540 432 407 506 392 461 481
    Y 7.3 9.6 11.2 5.1 5 5 5.9 11.5 14 12.3 8.8 13.9 11.4
    Zr 141 235 178 146 166 154 120 139 145 130 90 109 124
    Nb 6.3 4.4 5.6 4.1 4.1 3.9 7.4 9.4 12.7 9.6 10.1 11 8.6
    Mo 0.09 0.14 0.09 0.11 0.48 0.08 0.12 0.42 0.14 0.37 0.21 0.22 0.03
    Cd 0.04 0.03 0.06 .- .- .- 0.06 0.07 0.02 0.04 0.04 0.04 0.03
    Sn 0.5 0.6 0.6 0.7 0.5 0.5 0.6 0.5 0.8 0.9 1.1 1.1 0.4
    Sb 0.11 0.11 0.13 .- .- 0.09 0.21 0.53 0.2 0.14 0.27 0.18 0.11
    Cs 1 0.58 0.41 1.3 0.88 1.68 1.17 3.45 3.27 2.95 2.38 2.63 2.19
    Ba 2540 2410 1070 1510 1155 1285 1130 933 857 1010 829 824 881
    La 18.1 10.6 4.4 18.4 17.3 17.5 8.2 39.78 38.74 36.1 41.66 34.99 33.86
    Ce 35.3 22.1 13 35.7 33.1 33.9 15.6 78.06 73.42 68.2 73.46 66.09 63.61
    Pr 3.75 2.36 1.73 4.08 3.64 3.73 1.75 8.14 8.36 7.84 7.11 7.61 7.16
    Nd 13.5 8.7 7.1 15.4 13.3 13.5 6.2 27.29 28.79 27.36 22.75 26.19 24.89
    Sm 2.34 1.64 1.35 2.59 2.25 2.13 1.18 5.5 6.2 5.78 4.59 5.82 5.4
    Eu 0.67 0.53 0.46 0.59 0.49 0.52 0.47 1.18 1.17 1.29 1.01 1.18 1.18
    Gd 1.55 1.22 1.29 1.63 1.36 1.37 1.07 3.43 4.09 3.75 2.77 4.01 3.51
    Tb 0.23 0.19 0.19 0.18 0.16 0.16 0.15 0.49 0.56 0.51 0.38 0.52 0.46
    Dy 1.17 1.12 1.3 0.75 0.7 0.74 0.86 2.71 3.12 2.79 2.11 2.9 2.51
    Ho 0.22 0.24 0.3 0.14 0.12 0.13 0.16 0.5 0.61 0.52 0.4 0.57 0.48
    Er 0.61 0.7 0.97 0.37 0.3 0.34 0.45 1.36 1.63 1.4 1.12 1.59 1.29
    Tm 0.09 0.12 0.18 0.05 0.04 0.05 0.08 0.21 0.25 0.21 0.18 0.24 0.2
    Yb 0.59 0.96 1.42 0.31 0.25 0.3 0.47 1.38 1.73 1.44 1.32 1.63 1.31
    Lu 0.09 0.19 0.28 0.06 0.04 0.05 0.06 0.21 0.27 0.22 0.21 0.25 0.2
    Hf 3.6 4.2 3 4.1 4.4 4 3.3 4.9 5.36 4.54 3.55 4.26 4.47
    Ta 0.37 0.19 0.28 0.19 0.2 0.18 0.48 0.23 0.77 0.08 0.33 0.56 0.01
    Pb 29 25.2 14.1 32.3 30 30.7 35.4 16.7 17.4 12.3 14.2 13.5 18.2
    Th 1.27 0.89 0.32 3.31 2.94 2.63 1.23 16.36 19.83 14.41 15.18 17.18 18.92
    U 0.75 0.61 0.34 1.14 0.47 0.64 1.01 2.18 3.55 2.29 2.75 2.09 2.14
    K2O/Na2O 0.87 1.08 0.69 0.68 0.66 1.06 0.55 4.38 5.7 4.19 4.3 4.04 4.3
    (La/Yb)N 22.01 7.92 2.22 42.58 49.64 41.84 12.51 20.68 16.02 18.01 22.59 15.39 18.6
    (La/Sm)N 4.99 4.17 2.1 4.59 4.96 5.3 4.49 4.67 4.03 4.03 5.86 3.88 4.05
    (Gd/Yb)N 2.17 1.05 0.75 4.35 4.5 3.78 1.88 2.06 1.95 2.16 1.73 2.03 2.22
    Ce/Ce* 1.05 1.08 1.16 1.01 1.02 1.03 1.01 1.06 1 0.99 1.05 0.99 1
    Eu/Eu* 1.08 1.15 1.07 0.88 0.86 0.93 1.28 0.83 0.71 0.84 0.87 0.75 0.83
    ∑REE 78.21 50.67 33.97 80.25 73.05 74.42 36.7 170.2 169.0 157.4 159.1 153.6 146.0
    TZr (℃) 750 790 762 778 789 795 744 786 775 776 754 768 774
    样品号 B-0169-2 B-0169-3 B-0169-6 B-0169-7 B-0169-8 B-0169-9 JEW-1 JEW-2 ZJK-1 ZJK-5
    岩性 青羊沟花岗岩 井儿洼粗安岩 张家口组流纹岩
    SiO2 72.21 74.3 70 72.11 70.01 69.23 66.57 53.55 74.94 78.91
    TiO2 0.26 0.2 0.36 0.19 0.38 0.44 0.54 1.63 0.28 0.15
    Al2O3 14.34 13.45 15.18 14.98 15.11 15.21 13.53 18.25 15.5 11.45
    Fe2O3T 1.77 1.37 2.41 1.29 2.08 2.26 4.68 7.59 1.97 0.66
    MnO 0.05 0.05 0.08 0.03 0.05 0.06 0.06 0.14 0.01 0.02
    MgO 0.52 0.57 1.13 0.74 1.23 0.87 2.67 1.79 0.11 0.09
    CaO 0.26 0.23 0.64 0.26 0.65 0.64 2.78 6.42 0.14 0.09
    Na2O 4.53 4.06 5.63 4.69 4.54 4.51 1.47 3.88 0.1 4.21
    K2O 4.81 5.19 3.5 4.56 5.22 5.51 2.97 3.67 1.88 3.3
    P2O5 0.06 - 0.07 0.07 0.13 0.12 0.14 0.86 0.09 0.01
    Total 99.49 99.95 99.96 99.91 99.96 99.72 100.25 99.10 95.02 98.89
    Mg# 41 49 52 57 58 47 57 35 12 24
    Li 8.6 18.2 10.2 7.7 18.7 16.3 55.3 23.1 24.1 2.9
    Be 3.19 3.7 2.23 2.07 2.37 2.43 3.71 4.37 0.92 3.93
    Sc 2.5 3.3 3.5 1.3 5 5.5 10.0 13.9 4.9 2.9
    V 16 8 25 13 15 19 58 85 28 4
    Cr 4 6 4 4 4 5 21 1
    Co 1.8 1 2.6 1.5 2 2.5 9.6 10.2 1.4 0.4
    Ni 5 4.1 4.8 2.8 4 5.3 26.6 6.8 3.2 1.2
    Cu 3.5 5 15.8 4.2 4.2 2.9 17.2 10.3 5.4 0.9
    Zn 54 61 50 52 69 63 92.2 95.8 16 41
    Ga 19.4 18.8 17.2 19.7 19.6 19.7 19.4 23.5 17.1 22.8
    Rb 139.6 183.7 83.8 76.9 137.9 115 123 88 47 126
    Sr 251 79 575 676 279 269 171 1135 375 68.7
    Y 18.5 20.1 16.4 4.1 19.8 20.1 33.8 42.7 10.2 34.6
    Zr 221 118 309 45 101 112 298 786 144 337
    Nb 16.9 25.6 13.5 4.1 18.3 20.1 20.6 52.4 5 35.6
    Mo 1.22 0.71 - 0.27 1.41 0.82 0.87 1.20 0.4 0.07
    Cd 0.06 0.03 0.03 - 0.05 0.04 - - 0.03 0.09
    Sn 2.2 3 1.6 1.1 2 2.5 3.6 4.0 0.7 0.6
    Sb - - - - - - - - 0.41 0.13
    Cs 1.31 1.98 0.85 1.4 1.8 1.33 8.18 1.38 2.57 0.9
    Ba 489 398 959 1388 1551 1535 451 1169 620 140
    La 49.95 46.59 52.54 27.68 62.99 74.46 49.89 108.78 27.7 26.2
    Ce 89.11 88.92 103.3 49.1 135.6 145.7 96.4 222.8 52 67.2
    Pr 10.13 10.35 11.41 5.35 15.8 15.33 10.93 25.10 5.73 6.64
    Nd 33.44 35.61 38.6 18.67 51.28 50.15 39.98 93.58 20.1 22
    Sm 6.49 6.9 7.3 3.79 10.21 10.51 7.38 14.68 3 5.14
    Eu 0.67 0.94 1.23 0.78 1.9 1.9 1.13 3.35 0.95 0.25
    Gd 4.46 4.69 4.59 1.85 6.22 6.3 7.02 12.20 2.07 4.7
    Tb 0.63 0.65 0.59 0.19 0.78 0.8 1.02 1.49 0.32 0.87
    Dy 3.56 3.58 3.14 0.9 4.05 4.13 6.38 8.71 1.79 5.57
    Ho 0.68 0.68 0.58 0.15 0.72 0.75 1.24 1.61 0.36 1.16
    Er 1.91 1.91 1.56 0.39 1.9 1.9 3.82 4.72 1 3.17
    Tm 0.28 0.28 0.23 0.05 0.27 0.28 0.54 0.63 0.14 0.49
    Yb 1.87 1.85 1.53 0.34 1.74 1.79 3.48 4.09 0.96 3.25
    Lu 0.27 0.27 0.23 0.05 0.25 0.25 0.56 0.65 0.15 0.5
    Hf 7.65 4.8 8.35 1.46 3.61 4.17 7.92 15.16 3.5 10.6
    Ta 1.15 1.77 0.84 0.37 1.16 1.26 1.20 2.30 0.38 2.64
    Pb 48.9 25.8 30.3 32.4 18.8 16.4 26.62 14.29 16.3 5.8
    Th 15.59 13.35 11 4.13 10.96 13.07 13.44 11.56 3.8 30.4
    U 2.38 1 2.11 0.67 1.57 1.44 2.65 3.40 0.47 5.49
    K2O/Na2O 1.06 1.28 0.62 0.97 1.15 1.22 2.02 0.95 18.8 0.78
    (La/Yb)N 19.17 18.05 24.68 58.38 25.99 29.81 10.29 19.08 20.7 5.78
    (La/Sm)N 4.97 4.36 4.65 4.72 3.98 4.57 4.36 4.78 5.96 3.29
    (Gd/Yb)N 1.97 2.09 2.49 4.49 2.96 2.91 1.67 2.47 1.78 1.2
    Ce/Ce* 0.97 0.99 1.03 0.99 1.05 1.06 1.01 1.05 1.01 1.25
    Eu/Eu* 0.38 0.51 0.65 0.9 0.73 0.71 0.48 0.77 1.17 0.16
    ∑REE 203.5 203.2 226.8 109.3 293.7 314.3 229.8 502.4 116.3 147.1
    TZr (℃) 819 763 843 692 744 751 861 859 871 868
    注:“-”表示低于检测限; 空白表示没有测
    下载: 导出CSV
  •  

    Ahmad M, Solomon M and Walshe JL. 1987. Mineralogical and geochemical studies of the Emperor gold telluride deposit, Fiji. Economic Geology, 82(2): 345370 http://ci.nii.ac.jp/naid/10008463860

     

    Bao ZW, Zhao ZH, Zhang PH and Wang YX. 2003. REE, Sr, Nd, and Pb isotopic evidence for the petrogenesis of the Shuiquangou syenite complex in NW Hebei Province, China. Geological Review, 49(6): 596-604 (in Chinese with English abstract)

     

    Bao ZW, Sun WD, Li CJ and Zhao ZH. 2014. U-Pb dating of hydrothermal zircon from the Dongping gold deposit in North China: Constraints on the mineralization processes. Ore Geology Reviews, 61: 107-119 doi: 10.1016/j.oregeorev.2014.02.006

     

    Bao ZW, Li CJ and Zhao ZH. 2016. Metallogeny of the syenite-related Dongping gold deposit in the northern part of the North China Craton: A review and synthesis. Ore Geology Reviews, 73: 198-210 doi: 10.1016/j.oregeorev.2015.04.002

     

    Burnard PG, Hu R, Turner G and Bi XW. 1999. Mantle, crustal and atmospheric noble gases in ailaoshan gold deposits, Yunnan Province, China. Geochimica et Cosmochimica Acta, 63(10): 1595-1604 doi: 10.1016/S0016-7037(99)00108-8

     

    Cai MH, Peng ZA, Qu WJ, He ZY, Feng G, Zhang SQ, Xu M and Chen Y. 2011a. Geological characteristics and Re-Os dating of molybdenites in Chagandeersi molybdenum deposit, western Inner Mongolia. Mineral Deposits, 30(3): 377-384 (in Chinese with English abstract)

     

    Cai MH, Zhang ZG, Qu WJ, Peng ZA, Zhang SQ, Xu M, Chen Y and Wang XB. 2011b. Geological characteristics and Re-Os dating of the Chaganhua molybdenum deposit in Urad Rear Banner, western Inner Mongolia. Acta Geoscientica Sinica, 32(1): 64-68 (in Chinese with English abstract)

     

    Castillo PR, Janney PE and Solidum RU. 1999. Petrology and geochemistry of Camiguin Island, southern Philippines: Insights to the source of adakites and other lavas in a complex arc setting. Contributions to Mineralogy and Petrology, 134(1): 3351 doi: 10.1007/s004100050467

     

    Chappell BW and White AJR. 1992. I- and S-type granites in the Lachlan Fold Belt. Earth and Environmental Science Transactions of The Royal Society of Edinburgh, 83(1-2): 1-26 doi: 10.1017/S0263593300007720

     

    Chaussidon M and Lorand JP. 1990. Sulphur isotope composition of orogenic spinel lherzolite massifs from Ariege (North-Eastern Pyrenees, France): An ion microprobe study. Geochimica et Cosmochimica Acta, 54(10): 2835-2846 doi: 10.1016/0016-7037(90)90018-G

     

    Chen B, Tian W and Liu AK. 2008. Petrogenesis of the Xiaozhangjiakou mafic-ultramafic complex, North Hebei: Constraints from petrological, geochemical and Nd-Sr isotopic data. Geological Journal of Chinese Universities, 14(3): 295-303 (in Chinese with English abstract)

     

    Chen Q. 2013. Studies on fluid characteristics and mineralization mechanism of the Dabaiyang gold deposit, northwest of Hebei. Master Degree Thesis. Beijing: China University of Geosciences (Beijing) (in Chinese with English summary)

     

    Cisse M, Lü XB, Algeo TJ, Cao XF, Li H, Wei M, Yuan Q and Chen M. 2017. Geochronology and geochemical characteristics of the Dongping ore-bearing granite, North China: Sources and implications for its tectonic setting. Ore Geology Reviews, 89: 1091-1106 doi: 10.1016/j.oregeorev.2016.07.006

     

    Cook NJ, Ciobanu CL and Mao JW. 2009. Textural control on gold distribution in As-free pyrite from the Dongping, Huangtuliang and Hougou gold deposits, North China Craton (Hebei Province, China). Chemical Geology, 264(1-4): 101121

     

    Dai JZ, Mao JW, Zhao CS, Xie GQ, Yang FQ and Wang YT. 2009. New U-Pb and Re-Os age data and the geodynamic setting of the Xiaojiayingzi Mo (Fe) deposit, western Liaoning Province, Northeastern China. Ore Geology Reviews, 35(2): 235-244 doi: 10.1016/j.oregeorev.2008.10.001

     

    Decrée S, Demaiffe D, Tack L, Nimpagaritse G, De Paepe P, Boulvais P and Debaille V. 2019. The Neoproterozoic Upper Ruvubu alkaline plutonic complex (Burundi) revisited: Large-scale syntectonic emplacement, magmatic differentiation and late-stage circulations of fluids. Precambrian Research, 325: 150-171 doi: 10.1016/j.precamres.2019.02.023

     

    Defant MJ and Drummond MS. 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347(6294): 662-665 doi: 10.1038/347662a0

     

    Defant MJ and Drummond MS. 1993. Mount St. Helens: Potential example of the partial melting of the subducted lithosphere in a volcanic arc. Geology, 21(6): 547-550

     

    Deng J and Wang QF. 2016. Gold mineralization in China: Metallogenic provinces, deposit types and tectonic framework. Gondwana Research, 36: 219-274 doi: 10.1016/j.gr.2015.10.003

     

    DePaolo DJ. 1981. Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization. Earth and Planetary Science Letters, 53(2): 189-202 doi: 10.1016/0012-821X(81)90153-9

     

    Eby GN. 1992. Chemical subdivision of the A-type granitoids: Petrogenetic and tectonic implications. Geology, 20(7): 641-644 doi: 10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2

     

    Fan GH, Li JW, Deng XD, Gao WS and Li SY. 2021. Age and origin of the Dongping Au-Te deposit in the North China Craton revisited: Evidence from paragenesis, geochemistry, and in situ U-Pb geochronology of garnet. Economic Geology, 116(4): 963-985 doi: 10.5382/econgeo.4810

     

    Fan HR, Xie YH and Zhai MG. 2001. Ore-forming fluids in the Dongping gold deposit, northwestern Hebei Province. Science in China (Series D), 44(8): 748-757 doi: 10.1007/BF02907204

     

    Fan HR, Hu FF, Yang KF, Wang KY and Liu YS. 2009. Geochronology framework of Late Paleozoic dioritic-granitic plutons in the Bayan Obo area, Inner Mongolia, and tectonic significance. Acta Petrologica Sinica, 25(11): 2933-2938 (in Chinese with English abstract)

     

    Fu FJ. 2007. The study of mineralization in Huangtuliang gold deposit, Northwest Hebei. Master Degree Thesis. Shijiazhuang: Shijiazhuang University of Economics (in Chinese with English summary)

     

    Fu LB, Wei JH, Kusky TM, Chen HY, Tan J, Li YJ, Shi WJ, Chen C and Zhao SQ. 2012. The Cretaceous Duimiangou adakite-like intrusion from the Chifeng region, northern North China Craton: Crustal contamination of basaltic magma in an intracontinental extensional environment. Lithos, 134-135: 273-288 doi: 10.1016/j.lithos.2012.01.007

     

    Gao S, Luo TC, Zhang BR, Zhang HF, Han YW, Zhao ZD and Hu YK. 1998. Chemical composition of the continental crust as revealed by studies in East China. Geochimica et Cosmochimica Acta, 62(11): 1959-1975 doi: 10.1016/S0016-7037(98)00121-5

     

    Gao S, Rudnick RL, Yuan HL, Liu XM, Liu YS, Xu WL, Ling WL, Ayers J, Wang XC and Wang QH. 2004. Recycling lower continental crust in the North China craton. Nature, 432(7019): 892-897 doi: 10.1038/nature03162

     

    Gao YF, Santosh M, Hou ZQ, Wei RH, Ma GX, Chen ZK and Wu JL. 2012. High Sr/Y magmas generated through crystal fractionation: Evidence from Mesozoic volcanic rocks in the northern Taihang orogen, North China Craton. Gondwana Research, 22(1): 152168

     

    Han CM, Xiao WJ, Zhao GC, Sun M, Qu WJ and Du AD. 2009. A Re-Os study of molybdenites from the Lanjiagou Mo deposit of North China Craton and its geological significance. Gondwana Research, 16(2): 264-271 doi: 10.1016/j.gr.2009.01.001

     

    Hart CJ, Goldfarb RJ, Qiu YM, Snee L, Miller LD and Miller ML. 2002. Gold deposits of the northern margin of the North China Craton: Multiple Late Paleozoic-Mesozoic mineralizing events. Mineralium Deposita, 37(3): 326-351 doi: 10.1007/s00126-001-0239-2

     

    Hou WR. 2011. Constrast study on the Hadamengou gold deposit and Jinchanggouliang gold deposit, Inner Mongolia. Ph. D. Dissertation. Beijing: Chinese Academy of Geological Sciences (in Chinese with English summary)

     

    Huang F, Li SG, Dong F, He YS and Chen FK. 2008. High-Mg adakitic rocks in the Dabie orogen, central China: Implications for foundering mechanism of lower continental crust. Chemical Geology, 255(1-2): 1-13 doi: 10.1016/j.chemgeo.2008.02.014

     

    Huang WL and Wyllie PJ. 1981. Phase relationships of S-type granite with H2O to 35kbar: Muscovite granite from Harney Peak, South Dakota. Journal of Geophysical Research: Solid Earth, 86(B11): 10515-10529 doi: 10.1029/JB086iB11p10515

     

    Jian P, Liu DY, Kröner A, Windley BF, Shi YR, Zhang W, Zhang FQ, Miao LC, Zhang LQ and Tomurhuu D. 2010. Evolution of a Permian intraoceanic arc-trench system in the Solonker suture zone, Central Asian Orogenic Belt, China and Mongolia. Lithos, 118(1-2): 169-190 doi: 10.1016/j.lithos.2010.04.014

     

    Jiang N. 2005. Petrology and geochemistry of the Shuiquangou syenitic complex, northern margin of the North China Craton. Journal of the Geological Society, 162(1): 203-215 doi: 10.1144/0016-764903-144

     

    Jiang N. 2006. Hydrothermal alteration of chevkinite-(Ce) in the Shuiquangou syenitic intrusion, northern China. Chemical Geology, 227(1-2): 100-112 doi: 10.1016/j.chemgeo.2005.09.004

     

    Jiang N, Liu YS, Zhou WG, Yang JH and Zhang SQ. 2007. Derivation of Mesozoic adakitic magmas from ancient lower crust in the North China craton. Geochimica et Cosmochimica Acta, 71(10): 2591-2608 doi: 10.1016/j.gca.2007.02.018

     

    Jiang N, Zhang SQ, Zhou WG and Liu YS. 2009. Origin of a Mesozoic granite with A-type characteristics from the North China craton: Highly fractionated from I-type magmas? Contributions to Mineralogy and Petrology, 158(1): 113-130 doi: 10.1007/s00410-008-0373-2

     

    Jiang SH and Nie FJ. 1998. A comparison study on geological and geochemical features and ore genesis of the Xiaoyingpan and Dongping gold deposits, Hebei. Gold Geology, 4(4): 12-24 (in Chinese with English abstract)

     

    Jiang SH and Nie FJ. 2000. 40Ar/39Ar geochronology of the Shuiquangou alkaline complex and related gold deposits, northwestern Hebei, China. Geological Review, 46(6): 621-627 (in Chinese with English abstract)

     

    Jiang SH, Zhang LL, Liu YF, Liu CH, Kang H and Wang FX. 2018. Metallogeny of Xing-Meng Orogenic Belt and some related problems. Mineral Deposits, 37(4): 671-711 (in Chinese with English abstract)

     

    Jiang YH, Jiang SY, Zhao KD, Ni P, Ling HF and Liu DY. 2005. SHRIMP U-Pb zircon dating for lamprophyre from Liaodong Peninsula: Constraints on the initial time of Mesozoic lithosphere thinning beneath eastern China. Chinese Science Bulletin, 50(22): 2612-2620 doi: 10.1360/982005-373

     

    Li CJ and Bao ZW. 2012. Geochemical characteristics and geodynamic implications of the Early Cretaceous magmatisms in Zhangjiakou region, northwest Hebei Province, China. Geochimica, 41(4): 343-358 (in Chinese with English abstract)

     

    Li CM, Deng JF, Chen LH, Su SG, Li HM, Hu SL and Liu XM. 2010a. Two periods of zircon from Dongping gold deposit in Zhangjiakou-Xuanhua area, northern margin of North China: Constraints on metallogenic chronology. Mineral Deposits, 29(2): 265-275 (in Chinese with English anstract)

     

    Li CM, Deng JF, Su SG, Li HM and Liu XM. 2010b. Two stage zircon U-Pb ages of the potash altered rock in the Dongping gold deposit, Hebei Province, and their geological implications. Acta Geoscientica Sinica, 31(6): 843-852 (in Chinese with English abstract)

     

    Li CM, Deng JF., Su SG, Liu C and Liu XM. 2014. Zircon U-Pb chronology and Hf isotope in the western part of the Shuiquangou alkaline complex, northern Hebei Province. Acta Petrologica Sinica, 30(11): 3301-3314 (in Chinese with English abstract)

     

    Li H, Li JW, Algeo TJ, Wu JH and Cisse M. 2018. Zircon indicators of fluid sources and ore genesis in a multi-stage hydrothermal system: The Dongping Au deposit in North China. Lithos, 314-315: 463478 http://www.sciencedirect.com/science/article/pii/S0024493718302275

     

    Li R. 1992. Geological-geochemical features and metallogenic pattern of the Hougou gold deposit. Geology and Exploration, (3): 46-50 (in Chinese with English abstract)

     

    Li SZ and Jin GC. 2000. Geological characteristics and structural ore-controlling role of the Dongping gold deposit, Hebei Province. Acta Geoscientia Sinica, 21(1): 44-51 (in Chinese with English abstract)

     

    Li WB, Zhong RC, Xu C, Song B and Qu WJ. 2012. U-Pb and Re-Os geochronology of the Bainaimiao Cu-Mo-Au deposit, on the northern margin of the North China Craton, Central Asia Orogenic Belt: Implications for ore genesis and geodynamic setting. Ore Geology Reviews, 48: 139-150 doi: 10.1016/j.oregeorev.2012.03.001

     

    Li XY, Fan WM, Guo F, Wang YJ and Li CW. 2004. Modification of the lithospheric mantle beneath the northern North China Block by the Paleo-Asian Ocean: Geochemical evidence from mafic volcanic rocks of the Nandaling Formation in the Xishan area, Beijing. Acta Petrologica Sinica, 20(3): 557-566 (in Chinese with English abstract)

     

    Li YL, Zhou HW, Brouwer FM, Xiao WJ, Wijbrans JR and Zhong ZQ. 2014. Early Paleozoic to Middle Triassic bivergent accretion in the Central Asian Orogenic Belt: Insights from zircon U-Pb dating of ductile shear zones in central Inner Mongolia, China. Lithos, 205: 84-111 doi: 10.1016/j.lithos.2014.06.017

     

    Liu CH and Nie FJ. 2015. Permian magmatic sequences of the Bilihe gold deposit in central Inner Mongolia, China: Petrogenesis and tectonic significance. Lithos, 231: 3552

     

    Liu DY, Geng YS and Song B. 1997. Late Archean crustal accetion and reworking in northwestern Hebei Province: Isochronology evidence. Acta Geoscientia Sinica, 18(3): 226-232 (in Chinese with English abstract)

     

    Liu HT. 1999. Analysis of ore controlling factors of Huangtuliang gold deposit, Northwest Hebei Province. Journal of Precious Metallic Geology, 8(4): 209-216 (in Chinese with English abstract)

     

    Liu Q, Zhao GC, Sun M, Han YG, Eizenhofer PR, Hou WZ, Zhang XR, Zhu YL, Wang B, Liu DX and Xu B. 2016. Early Paleozoic subduction processes of the Paleo-Asian Ocean: Insights from geochronology and geochemistry of Paleozoic plutons in the Alxa Terrane. Lithos, 262: 546-560 doi: 10.1016/j.lithos.2016.07.041

     

    Liu Y, Liu HC and Li XH. 1996. Simultaneous and precise determination of 40 trace elements in rock samples using ICP-MS. Geochimica, 25(6): 552-558 (in Chinese with English abstract)

     

    Liu YF, Nie FJ, Jiang SH, Hou WR, Liang QL, Zhang K and Liu Y. 2012. Geochronology of Zhunsujihua molybdenum deposit in Sonid Left Banner, Inner Mongolia, and its geological significance. Mineral Deposits, 31(1): 119-128 (in Chinese with English abstract)

     

    Liu YF and Jiang SH. 2017. Mo mineralization in Xing'an-Mongolian orogen and north margin of Chinacraton: Review, question and a preliminary genetic model. Mineral Deposits, 36(3): 557-594 (in Chinese with English abstract)

     

    Liu YS, Hu ZC, Gao S, Günther D, Xu J, Gao CG and Chen HH. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology, 257(1-2): 34-43 doi: 10.1016/j.chemgeo.2008.08.004

     

    Liu YS, Gao S, Hu ZC, Gao CG, Zong KQ and Wang DB. 2010. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths. Journal of Petrology, 51(1-2): 537-571 doi: 10.1093/petrology/egp082

     

    Lu DL, Luo XQ, Wang JJ, Zhang SH and Zheng BY. 1993. The metallogenic epoch of the Dongping gold deposit. Mineral Deposits, 12(2): 182-188 (in Chinese with English abstract)

     

    Lu FX, Zheng JP, Shao JA, Zhang RS, Chen MH and Yu CM. 2006. Asthenospheric upwelling and lithospheric thinning in late Cretaceous-Cenozoic in eastern North China. Earth Science Frontiers, 13(2): 86-92 (in Chinese with English abstract)

     

    Ludwig KR. 2003. User's Manual for Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley: Berkeley Geochronology Center

     

    Luo ZK, Miao LC and Guan K. 2000. Discussion on the metallogenetic epoch of gold deposit on north fringe of North China platform. Gold Geology, 6(2): 70-76 (in Chinese with English abstract)

     

    Ma Q, Zheng JP, Xu YG, Griffin WL and Zhang RS. 2015. Are continental "adakites" derived from thickened or foundered lower crust? Earth and Planetary Science Letters, 419: 125-133 doi: 10.1016/j.epsl.2015.02.036

     

    Ma YS, Cui SQ, Zhao Y, Zeng QL and Wu ML. 2002. The transformation process of Mesozoic-cenozoic tectonic regime in the north of North China. Journal of Geomechanics, 8(1): 15-25 (in Chinese with English abstract)

     

    Mao JW, Li YQ, Goldfarb R, He Y and Zaw K. 2003. Fluid inclusion and noble gas studies of the Dongping gold deposit, Hebei Province, China: A mantle connection for mineralization? Economic Geology, 98(3): 517-534

     

    Mao JW, Wang YT, Zhang ZH, Yu JJ and Niu BG. 2003. Geodynamic settings of Mesozoic large-scale mineralization in North China and adjacent areas: Implication from the highly precise and accurate ages of metal deposits. Science in China (Series D), 46(8): 838-851

     

    Mao JW, Xie GQ, Zhang ZH, Li XF, Wang YT, Zhang CQ and Li YF. 2005. Mesozoic large-scale metallogenic pulses in North China and corresponding geodynamic setting. Acta Petrologica Sinica, 21(1): 169-188 (in Chinese with English abstract)

     

    Mark DF, Stuart FM and de Podesta M. 2011. New high-precision measurements of the isotopic composition of atmospheric argon. Geochimica et Cosmochimica Acta, 75(23): 74947501

     

    Martin H, Smithies RH, Rapp R, Moyen JF and Champion D. 2005. An overview of adakite, tonalite-trondhjemite-granodiorite (TTG), and sanukitoid: Relationships and some implications for crustal evolution. Lithos, 79(1-2): 1-24 doi: 10.1016/j.lithos.2004.04.048

     

    Miao LC, Qiu YM, McNaughton N, Luo ZK, Groves D, Zhai YS, Fan WM, Zhai MG and Guan K. 2002. SHRIMP U-Pb zircon geochronology of granitoids from Dongping area, Hebei Province, China: Constraints on tectonic evolution and geodynamic setting for gold metallogeny. Ore Geology Reviews, 19(3-4): 187-204 doi: 10.1016/S0169-1368(01)00041-5

     

    Moyen JF. 2009. High Sr/Y and La/Yb ratios: The meaning of the "adakitic signature". Lithos, 112(3-4): 556-574 doi: 10.1016/j.lithos.2009.04.001

     

    Nie FJ. 1998. Geology and origin of the Dongping alkalic-type gold deposit, Northern Hebei province, People's Republic of China. Resource Geology, 48(3): 139-158 doi: 10.1111/j.1751-3928.1998.tb00013.x

     

    Ohmoto H. 1972. Systematics of sulfur and carbon isotopes in hydrothermal ore deposits. Economic Geology, 67(5): 551-578 doi: 10.2113/gsecongeo.67.5.551

     

    Riishuus MS, Peate DW, Tegner C, Wilson JR, Brooks CK and Waight TE. 2005. Petrogenesis of syenites at a rifted continental margin: Origin, contamination and interaction of alkaline mafic and felsic magmas in the Astrophyllite Bay Complex, East Greenland. Contributions to Mineralogy and Petrology, 149(3): 350-371 doi: 10.1007/s00410-005-0655-x

     

    Scherbarth NL and Spry PG. 2006. Mineralogical, petrological, stable isotope, and fluid inclusion characteristics of the Tuvatu gold-silver telluride deposit, Fiji: Comparisons with the emperor deposit. Economic Geology, 101(1): 135-158 doi: 10.2113/gsecongeo.101.1.135

     

    Shangguan S, Peate IU, Tian W and Xu Y. 2016. Re-evaluating the geochronology of the Permian Tarim magmatic province: Implications for temporal evolution of magmatism. Journal of the Geological Society, 173(1): 228-239 doi: 10.1144/jgs2014-114

     

    Shao JA, He GQ and Tang KD. 2015. The evolution of Permian continental crust in northern part of North China. Acta Petrologica Sinica, 31(1): 47-55 (in Chinese with English abstract)

     

    Shen JF, Santosh M, Li SR., Li CP, Zhang JQ, Zhang SQ, Alam M, Wang YH and Xu KX. 2020. He-Ar, S, Pb and O isotope geochemistry of the Dabaiyang gold deposit: Implications for the relationship between gold metallogeny and destruction of the North China Craton. Ore Geology Reviews, 116: 103229 doi: 10.1016/j.oregeorev.2019.103229

     

    Shi LS, Rao YX, Song RX and Wen JH. 2007. Geological characteristics of isotopes and inclusions in gold accumulated area of Zhangjiakou, Hebei Province. Mineral Resources and Geology, 21(3): 219-227 (in Chinese with English abstract)

     

    Shi YR, Liu DY, Miao LC, Zhang FQ, Jian P, Zhang W, Hou KJ and Xu JY. 2010. Devonian A-type granitic magmatism on the northern margin of the North China Craton: SHRIMP U-Pb zircon dating and Hf-isotopes of the Hongshan granite at Chifeng, Inner Mongolia, China. Gondwana Research, 17(4): 632641

     

    Song GR and Zhao ZH. 1996. Geology of Dongping Alkaline Complex-Hosted Gold Deposit in Hebei Province. Beijing: Seismological Press (in Chinese with English abstract)

     

    Song RX, Wei MH, Wang JS et al. 2013. Geology and Ores in the Zhangjiakou District. Beijing: Geological Publishing House (in Chinese)

     

    Song Y, Jiang SH, Bagas L, Li C, Hu JZ, Zhang Q, Zhou W and Ding HY. 2016. The geology and geochemistry of Jinchangyu gold deposit, North China Craton: Implications for metallogenesis and geodynamic setting. Ore Geology Reviews, 73: 313-329 doi: 10.1016/j.oregeorev.2014.10.031

     

    Spry PG, Paredes MM, Foster F, Truckle JS and Chadwick TH. 1996. Evidence for a genetic link between gold-silver telluride and porphyry molybdenum mineralization at the Golden Sunlight deposit, Whitehall, Montana: Fluid inclusion and stable isotope studies. Economic Geology, 91(3): 507-526 doi: 10.2113/gsecongeo.91.3.507

     

    Stern RA and Hanson GN. 1991. Archean high-Mg granodiorite: A derivative of light rare earth element enriched monzodiorite of mantle origin. Journal of Petrology, 32(1): 201238

     

    Stuart FM, Burnard PG, Taylor RP and Turner G. 1995. Resolving mantle and crustal contributions to ancient hydrothermal fluids: He-Ar isotopes in fluid inclusions from Dae Hwa W-Mo mineralisation, South Korea. Geochimica et Cosmochimica Acta, 59(22): 46634673

     

    Sun JF and Yang JH. 2009. Early Cretaceous A-type granites in the Eastern North China Block with relation to destruction of the craton. Earth Science (Journal of China University of Geosciences), 34(1): 137-147 (in Chinese with English abstract) doi: 10.3799/dqkx.2009.013

     

    Sun SS and McDonough WF. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: Saunders AD and Norry MJ (eds. ). Magmatism in the Ocean Basins. Geological Society, London, Special Publications, 42(1): 313-345 doi: 10.1144/GSL.SP.1989.042.01.19

     

    Sutcliffe RH, Smith AR, Doherty W and Barnett RL. 1990. Mantle derivation of Archean Amphibole-bearing granitoid and associated mafic rocks: Evidence from the Southern Superior Province, Canada. Contributions to Mineralogy and Petrology, 105(3): 255-274 doi: 10.1007/BF00306538

     

    Tao LX, Zhen SM, Bai HJ, Wang J, Wang DZ and Zha ZJ. 2020. Pyrite trace element composition and S-Pb isotope characters of the Dabaiyang gold deposit, Hebei Province. Journal of Jilin University (Earth Science Edition), 50(5): 1582-1598 (in Chinese with English abstract)

     

    Tian W, Chen B, Liu CQ and Zhang HF. 2007. Zircon U-Pb age and Hf isotopic composition of the Xiaozhangjiakou ultramafic pluton in northern Hebei. Acta Petrologica Sinica, 23(3): 583-590 (in Chinese with English abstract)

     

    Vernon RH. 2004. A Practical Guide to Rock Microstructure. New York: Cambridge University Press

     

    Wang DZ, Liu JJ, Zhai DG, Carranza EJM, Wang YH, Zhen SM, Wang J, Wang JP, Liu ZJ and Zhang FF. 2019a. Mineral paragenesis and ore-forming processes of the Dongping gold deposit, Hebei Province, China. Resource Geology, 69(3): 287-313 doi: 10.1111/rge.12202

     

    Wang DZ, Liu JJ, Zhai DG, Zhen SM, Wang J and Yang XA. 2019b. New discovery of molybdenite in the Dongping gold deposit, Hebei province, China and its Re-Os geochronological implications. Acta Geologica Sinica, 93(3): 769-770 doi: 10.1111/1755-6724.13841

     

    Wang DZ, Liu JJ, Zhai DG, de Fourestier J, Wang YH, Zhen SM, Wang JP, Liu ZJ and Zhang FF. 2020. Textures and formation of microporous gold in the Dongping gold deposit, Hebei Province, China. Ore Geology Reviews, 120: 103437 doi: 10.1016/j.oregeorev.2020.103437

     

    Wang DZ, Liu JJ, Zhai DG, Zhen SM and Wang J. 2020. Study on molybdenite Re-Os and zircon U-Pb ages of the Dongping tellurium-gold deposit in Hebei Province. Earth Science Frontiers, 27(2): 405-419 (in Chinese with English abstract)

     

    Wang DZ, Zhen SM, Liu JJ, Carranza EJM, Wang J, Zha ZJ, Li YS and Bai HJ. 2021. Mineral paragenesis and hydrothermal evolution of the Dabaiyang tellurium-gold deposit, Hebei Province, China: Constraints from fluid inclusions, H-O-He-Ar isotopes, and physicochemical conditions. Ore Geology Reviews, 130: 103904 doi: 10.1016/j.oregeorev.2020.103904

     

    Wang JP, Liu YS, Dong XF, Li ZJ, Peng H, Wang LJ, Ding YC, Yang YD, Meng XG, Jia HJ, Liu ZB, Liu JM and Wang HC. 1992. Study on Ore-Controlling Tectonics of Jinchanggouliang Gold Deposit, Inner Mongolia. Beijing: Geological Publishing House (in Chinese with English abstract)

     

    Wang L, Wang GH, Lei SB, Chang CJ, Hou WR, Jia LQ, Zhao GM and Chen HJ. 2015. Re-Os dating of molybdenites from the Houshihua gold deposit in Wuchuan County, Inner Mongolia and its geological significance. Geology and Exploration, 51(3): 422-431 (in Chinese with English abstract)

     

    Wang SL. 1986. Study of the genesis of Zhangjiakou gold deposit. Acta Scientiarum Naturalium, Universitatis Pekinensis, (4): 81-89 (in Chinese with English abstract)

     

    Wang Y, Jiang XM and Wang ZK. 1990. Characteristics of lead and sulfur isorope of the gold deposits in Zhangjiakou Xuanhua area Hebei Province. Contributions to Geology and Mineral Resources Research, 5(2): 66-75 (in Chinese with English abstract)

     

    Wang ZK, Jiang XM, Wang Y and Shang MY. 1992. A comparative analysis on geological-geochemical features of the Xiaoyingpan and Dongping gold deposits, Hebei. Geology and Exploration, (7): 14-20 (in Chinese with English abstract)

     

    Wei ZL, Zhang H, Liu XM and Zhang YQ. 2008. LA-ICP-MS dating and geological meaning of the Zhangjiakou Formation volcanic rocks, Zhangjiakou area. Progress in Natural Science, 18(5): 523-530 (in Chinese) doi: 10.1016/j.pnsc.2007.12.005

     

    Whalen JB, Currie KL and Chappell BW. 1987. A-type granites: Geochemical characteristics, discrimination and petrogenesis. Contributions to Mineralogy and Petrology, 95(4): 407-419 doi: 10.1007/BF00402202

     

    Windley BF, Alexeiev D, Xiao WJ, Kroner A and Badarch G. 2007. Tectonic models for accretion of the Central Asian Orogenic Belt. Journal of the Geological Society, 164: 31-47 doi: 10.1144/0016-76492006-022

     

    Wu FY, Xu YG, Gao S and Zheng JP. 2008. Lithospheric thinning and destruction of the North China Craton. Acta Petrologica Sinica, 24(6): 1145-1174 (in Chinese with English abstract)

     

    Wu FY, Liu XC, Ji WQ, Wang JM and Yang L. 2017. Highly fractionated granites: Recognition and research. Science China (Earth Sciences), 60(7): 1201-1219 doi: 10.1007/s11430-016-5139-1

     

    Wu SS. 2009. Research on ore-formation and ore-controlling structure of Zhongshangou gold deposit in Chongli County, Hebei Province. Master Degree Thesis. Shijiazhuang: Shijiazhuang University of Economics (in Chinese with English summary)

     

    Wyllie PJ and Sekine T. 1982. The formation of mantle phlogopite in subduction zone hybridization. Contributions to Mineralogy and Petrology, 79(4): 375-380 doi: 10.1007/BF01132067

     

    Xiao WJ, Windley BF, Hao J and Zhai MG. 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt. Tectonics, 22(6): 1069

     

    Xu YG, Li HY, Pang CJ and He B. 2009. On the timing and duration of the destruction of the North China Craton. Chinese Science Bulletin, 54(19): 3379-3396

     

    Yang F, Santosh M, Kim SW, Zhou HY and Jeong YJ. 2020. Late Mesozoic intraplate rhyolitic volcanism in the North China Craton: Far-field effect of the westward subduction of the Paleo-Pacific Plate. Geological Society of America Bulletin, 132(1-2): 291-309 doi: 10.1130/B35123.1

     

    Yang JH, Wu FY, Chung SL, Wilde SA, Chu MF, Lo CH and Song B. 2005. Petrogenesis of Early Cretaceous intrusions in the Sulu ultrahigh-pressure orogenic belt, East China and their relationship to lithospheric thinning. Chemical Geology, 222(34): 200231

     

    Yang JH, Wu FY, Liu XM and Xie LW. 2005. Zircon U-Pb ages and Hf isotopes and their geological significance of the Miyun rapakivi granites from Beijing, China. Acta Petrologica Sinica, 21(6): 1633-1644 (in Chinese with English abstract)

     

    Yang JH, Wu FY, Shao JA, Xie LW and Liu XM. 2006. In-situ U-Pb dating and Hf isotopic analyses of zircons from volcanic rocks of the Houcheng and Zhangjiakou Formations in the Zhang-Xuan area, Northeast China. Earth Science (Journal of China University of Geosciences), 31(1): 71-80 (in Chinese with English abstract)

     

    Yang ZM, Chang ZS, Hou ZQ and Meffre S. 2016. Age, igneous petrogenesis, and tectonic setting of the Bilihe gold deposit, China, and implications for regional metallogeny. Gondwana Research, 34: 296314

     

    Yin JZ and Shi HY. 1995. Geology of Gold Ore Deposits in Zhangjiakou-Xuanhua Region, Hebei Province, China. Beijing: Geological Publishing House (in Chinese)

     

    Yu B, Zeng QD, Frimmel HE, Qiu HC, Li QL, Yang JH, Wang YB, Zhou LL, Chen PW and Li JP. 2020. The 127Ma gold mineralization in the Wulong deposit, Liaodong Peninsula, China: Constraints from molybdenite Re-Os, monazite U-Th-Pb, and zircon U-Pb geochronology. Ore Geology Reviews, 121: 103542 doi: 10.1016/j.oregeorev.2020.103542

     

    Zeng QD, Liu JM, Zhang ZL, Qin F, Chen WJ, Zhang RB, Yu CM and Ye J. 2009. Ore-forming time of the Jiguanshan porphyry molybdenum deposit, northern margin of North China Craton and the Indosinian mineralization. Acta Petrologica Sinica, 25(2): 393-398 (in Chinese with English abstract)

     

    Zeng QD, Sun Y, Duan XX and Liu JM. 2013. U-Pb and Re-Os geochronology of the Haolibao porphyry Mo-Cu deposit, NE China: Implications for a Late Permian tectonic setting. Geological Magazine, 150(6): 975-985 doi: 10.1017/S0016756813000186

     

    Zeng QD, Wang YB, Yang JH, Guo YP, Yu B, Zhou LL and Qiu HC. 2021. Spatial-temporal distribution and tectonic setting of gold deposits in the northern margin gold belt of the North China Craton. International Geology Review, 63(8): 941-972 doi: 10.1080/00206814.2020.1737839

     

    Zhai MG and Peng P. 2007. Paleoproterozoic events in the North China Craton. Acta Petrologica Sinica, 23(11): 2665-2682 (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200711002.htm

     

    Zhai MG. 2010. Tectonic evolution and metallogenesis of North China Craton. Mineral Deposits, 29(1): 24-36 (in Chinese with English abstract)

     

    Zhang C, Ma CQ and Holtz F. 2012. Partial melting of hydrous lower continental crust: Discussion on the petrogenesis of C-type adakites from the Dabie Orogen. Geological Journal of China Universities, 18(1): 41-51 (in Chinese with English abstract)

     

    Zhang C, Guo W, Xu ZY, Liu ZH, Liu YJ and Lei CC. 2014. Study on geochronology, petrogenesis and tectonic implications of monzogranite from the Yanbian area, eastern Jilin Province. Acta Petrologica Sinica, 30(2): 512-526 (in Chinese with English abstract)

     

    Zhang LL, Jiang SH, Li HM, Wu D and Kang H. 2019. Metallogenic and petrogenic geochronology and geochemical features of the ore-related granite in the Sadaigoumen Mo Deposit, Fengning, Hebei Province. Acta Geoscientica Sinica, 40(5): 708-724 (in Chinese with English abstract)

     

    Zhang QQ, Zhang SH, Zhao Y and Liu JM. 2018. Devonian alkaline magmatic belt along the northern margin of the North China Block: Petrogenesis and tectonic implications. Lithos, 302-303: 496-518 doi: 10.1016/j.lithos.2018.01.019

     

    Zhang SH, Zhao Y, Song B and Liu DY. 2007. Petrogenesis of the Middle Devonian Gushan diorite pluton on the northern margin of the North China block and its tectonic implications. Geological Magazine, 144(3): 553-568 doi: 10.1017/S0016756807003275

     

    Zhang SH, Zhao Y, Kröner A, Liu XM, Xie LW and Chen FK. 2009a. Early Permian plutons from the northern North China Block: Constraints on continental arc evolution and convergent margin magmatism related to the Central Asian Orogenic Belt. International Journal of Earth Sciences, 98(6): 1441-1467 doi: 10.1007/s00531-008-0368-2

     

    Zhang SH, Zhao Y, Liu XC, Liu DY, Chen, FK, Xie LW and Chen HH. 2009b. Late Paleozoic to Early Mesozoic mafic-ultramafic complexes from the northern North China Block: Constraints on the composition and evolution of the lithospheric mantle. Lithos, 110(1-4): 229-246 doi: 10.1016/j.lithos.2009.01.008

     

    Zhang SH, Zhao Y, Song B, Hu JM, Liu SW, Yang YH, Chen FK, Liu XM and Liu J. 2009c. Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications. Geological Society of America Bulletin, 121(1-2): 181-200

     

    Zhang SH, Zhao Y, Ye H, Hou KJ and Li CF. 2012. Early Mesozoic alkaline complexes in the northern North China Craton: Implications for cratonic lithospheric destruction. Lithos, 155: 1-18 doi: 10.1016/j.lithos.2012.08.009

     

    Zhang SH, Zhao Y, Ye H, Liu JM and Hu ZC. 2014a. Origin and evolution of the Bainaimiao arc belt: Implications for crustal growth in the southern Central Asian orogenic belt. Geological Society of America Bulletin, 126(9-10): 1275-1300 doi: 10.1130/B31042.1

     

    Zhang SH, Zhao Y, Davis GA, Ye H and Wu F. 2014b. Temporal and spatial variations of Mesozoic magmatism and deformation in the North China Craton: Implications for lithospheric thinning and decratonization. Earth-Science Reviews, 131: 49-87 doi: 10.1016/j.earscirev.2013.12.004

     

    Zhang T, Chen ZY, Xu LQ and Chen ZH. 2009. The Re-Os isotopic dating of molybdenite from the Dasuji molybdenum deposit in Zhuozi County of Inner Mongolia and its geological significance. Rock and Mineral Analysis, 28(3): 279-282 (in Chinese with English abstract)

     

    Zhang XH and Zhai MG. 2010. Magmatism and its metallogenetic effects during the Paleozoic continental crustal construction in northern North China: An overview. Acta Petrologica Sinica, 26(5): 1329-1341 (in Chinese with English abstract)

     

    Zhang XH, Zhang HF, Jiang N, Zhai MG and Zhang YB. 2010. Early Devonian alkaline intrusive complex from the northern North China craton: A petrological monitor of post-collisional tectonics. Journal of the Geological Society, 167(4): 717-730 doi: 10.1144/0016-76492009-110

     

    Zhang YM, Gu XX, Xiang ZL, Liu RP, Cheng WB and Wang XL. 2017. Magmatic hydrothermal origin of the Hadamengou-Liubagou Au-Mo deposit, Inner Mongolia, China: Constrains on geology, stable and Re-Os isotopes. Ore Geology Reviews, 86: 172-195 doi: 10.1016/j.oregeorev.2017.01.029

     

    Zhang ZC. 1995. Origin of Shuiquangou complex in Northern Hebei Province and a study of its relation to the gold mineralization. Ph. D. Dissertation. Beijing: Chinese Academy of Geological Sciences (in Chinese with English summary)

     

    Zhang ZC and Mao JW. 1995. Geology and geochemistry of the Dongping gold telluride deposit, Heibei Province, North China. International Geology Review, 37(12): 1094-1108 doi: 10.1080/00206819509465441

     

    Zhang ZC and Chen HX. 1997. Geology and petrology of Shuiquangou complex, northern Hebei Province. 6(2): 81-92 (in Chinese with English abstract)

     

    Zhao GC, Wilde SA, Li SZ, Sun M, Grant ML and Li XP. 2007. U-Pb zircon age constraints on the Dongwanzi ultramafic-mafic body, North China, confirm it is not an Archean ophiolite. Earth and Planetary Science Letters, 255(1-2): 85-93 doi: 10.1016/j.epsl.2006.12.007

     

    Zhao GC and Zhai MG. 2013. Lithotectonic elements of Precambrian basement in the North China Craton: Review and tectonic implications. Gondwana Research, 23(4): 1207-1240 doi: 10.1016/j.gr.2012.08.016

     

    Zhao Y, Zhai MG, Chen H and Zhang SH. 2017. Paleozoic-early Jurassic tectonic evolution of North China Craton and its adjacent orogenic belts. Geology in China, 44(1): 44-60 (in Chinese with English abstract)

     

    Zhao ZH, Bao ZW and Qiao YL. 2010. A peculiar composite M- and W-type REE tetrad effect: Evidence from the Shuiquangou alkaline syenite complex, Hebei Province, China. Chinese Science Bulletin, 55(22): 2684-2696

     

    Zhen SM, Wang QF, Wang DZ, Carranza EJM, Liu J, Pang Z, Cheng Z, Xue J, Wang J and Zha ZJ. 2020. Genesis of the Zhangquanzhuang gold deposit in the northern margin of North China Craton: constraints from deposit geology and ore isotope geochemistry. Ore Geology Reviews, 122: 103511 doi: 10.1016/j.oregeorev.2020.103511

     

    Zhen SM, Zha ZJ, Wang DZ, Liu JJ, Pang ZS, Cheng ZZ, Xue JL, Wang J, Bai HJ, Li Y, Chen C. 2021. Characteristics of ore-forming fluids of the Zhongshangou gold deposit, Zhangjiakou-Xuanhua area, Hebei Province, and its limitation on the intrusive rock related telluride-gold deposits. Geology in China: 1-27 (in Chinese with English abstract)

     

    Zhu RX, Chen L, Wu FY and Liu JL. 2011. Timing, scale and mechanism of the destruction of the North China Craton. Science China (Earth Sciences), 54(6): 789-797 doi: 10.1007/s11430-011-4203-4

     

    Zhu RX, Yang JH and Wu FY. 2012. Timing of destruction of the North China Craton. Lithos, 149: 51-60 doi: 10.1016/j.lithos.2012.05.013

     

    包志伟, 赵振华, 张佩华, 王一先. 2003. 张家口水泉沟正长岩杂岩体成因的REE和Sr、Nd、Pb同位素证据. 地质论评, 49(6): 596-604 doi: 10.3321/j.issn:0371-5736.2003.06.006

     

    蔡明海, 彭振安, 屈文俊, 贺钟银, 冯罡, 张诗启, 徐明, 陈艳. 2011a. 内蒙古乌拉特后旗查干德尔斯钼矿床地质特征及Re-Os测年. 矿床地质, 30(3): 377-384 https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201103002.htm

     

    蔡明海, 张志刚, 屈文俊, 彭振安, 张诗启, 徐明, 陈艳, 王显彬. 2011b. 内蒙古乌拉特后旗查干花钼矿床地质特征及Re-Os测年. 地球学报, 32(1): 64-68 https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201101010.htm

     

    陈斌, 田伟, 刘安坤. 2008. 冀北小张家口基性-超基性杂岩的成因: 岩石学、地球化学和Nd-Sr同位素证据. 高校地质学报, 14(3): 295-303 doi: 10.3969/j.issn.1006-7493.2008.03.002

     

    陈茜. 2013. 冀西北大白阳金矿成矿流体及成矿机制研究. 硕士学位论文. 北京: 中国地质大学(北京)

     

    范宏瑞, 胡芳芳, 杨奎锋, 王凯怡, 刘勇胜. 2009. 内蒙古白云鄂博地区晚古生代闪长质-花岗质岩石年代学框架及其地质意义. 岩石学报, 25(11): 2933-2938 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20091122&journal_id=ysxb

     

    付方建. 2007. 冀西北黄土梁金矿成矿规律研究. 硕士学位论文. 石家庄: 石家庄经济学院

     

    侯万荣. 2011. 内蒙古哈达门沟金矿床与金厂沟梁金矿床对比研究. 博士学位论文. 北京: 中国地质科学院

     

    江思宏, 聂凤军. 1998. 河北小营盘与东坪金矿地质地球化学特征对比及矿床成因探讨. 黄金地质, 4(4): 12-24 https://www.cnki.com.cn/Article/CJFDTOTAL-HJDZ804.002.htm

     

    江思宏, 聂凤军. 2000. 冀西北水泉沟杂岩体及与其有关金矿床的40Ar/39Ar同位素年代学研究. 地质论评, 46(6): 621-627 doi: 10.3321/j.issn:0371-5736.2000.06.010

     

    江思宏, 张莉莉, 刘翼飞, 刘春花, 康欢, 王丰翔. 2018. 兴蒙造山带成矿规律及若干科学问题. 矿床地质, 37(4): 671-711 https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201804001.htm

     

    姜耀辉, 蒋少涌, 赵葵东, 倪培, 凌洪飞, 刘敦一. 2005. 辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约. 科学通报, 50(19): 2161-2168 doi: 10.3321/j.issn:0023-074X.2005.19.016

     

    李创举, 包志伟. 2012. 冀西北早白垩世岩浆岩的地球化学特征及其地球动力学背景. 地球学报, 41(4): 343-358 https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX201204004.htm

     

    李长民, 邓晋福, 陈立辉, 苏尚国, 李惠民, 胡森林, 刘新秒. 2010a. 华北北缘张宣地区东坪金矿中的两期锆石: 对成矿年龄的约束. 矿床地质, 29(2): 265-275 https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201002008.htm

     

    李长民, 邓晋福, 苏尚国, 李惠民, 刘新秒. 2010b. 河北省东坪金矿钾质蚀变岩中的两期锆石年代学研究及意义. 地球学报, 31(6): 843-852 https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201006014.htm

     

    李长民, 邓晋福, 苏尚国, 刘翠, 刘新秒. 2014. 冀北水泉沟岩体西段锆石U-Pb年代学及Hf同位素研究. 岩石学报, 30(11): 3301-3314 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20141114&journal_id=ysxb

     

    李瑞. 1992. 后沟金矿地质地球化学特征及其成矿模式初步探讨. 地质与勘探, (3): 46-50 https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT199203009.htm

     

    李少众, 靳光成. 2000. 东坪金矿床地质特征及构造控矿作用. 地球学报, 21(1): 44-51 doi: 10.3321/j.issn:1006-3021.2000.01.007

     

    李晓勇, 范蔚茗, 郭锋, 王岳军, 李超文. 2004. 古亚洲洋对华北陆缘岩石圈的改造作用: 来自于西山南大岭组中基性火山岩的地球化学证据. 岩石学报, 20(3): 557-566 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20040354&journal_id=ysxb

     

    刘敦一, 耿元生, 宋彪. 1997. 冀西北地区晚太古代大陆地壳的增生和再造——同位素年代学证据. 地球学报, 18(3): 226-232 https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB703.000.htm

     

    刘海田. 1999. 冀西北黄土梁金矿控矿因素分析. 贵金属地质, 8(4): 209-216 https://www.cnki.com.cn/Article/CJFDTOTAL-GJSD199904002.htm

     

    刘颖, 刘海臣, 李献华. 1996. 用ICP-MS准确测定岩石样品中的40余种微量元素. 地球化学, 25(6): 552-558 doi: 10.3321/j.issn:0379-1726.1996.06.004

     

    刘翼飞, 聂凤军, 江思宏, 侯万荣, 梁清玲, 张可, 刘勇. 2012. 内蒙古苏尼特左旗准苏吉花钼矿床成岩成矿年代学及其地质意义. 矿床地质, 31(1): 119-128 doi: 10.3969/j.issn.0258-7106.2012.01.010

     

    刘翼飞, 江思宏. 2017. 兴蒙造山带及华北板块北缘钼矿化: 进展、规律、问题与成因初探. 矿床地质, 36(3): 557-594 https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201703003.htm

     

    卢德林, 罗修泉, 汪建军, 张思红, 郑宝英. 1993. 东坪金矿成矿时代研究. 矿床地质, 12(2): 182-188 https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ199302009.htm

     

    路凤香, 郑建平, 邵济安, 张瑞生, 陈美华, 余淳梅. 2006. 华北东部中生代晚期-新生代软流圈上涌与岩石圈减薄. 地学前缘, 13(2): 86-92 doi: 10.3321/j.issn:1005-2321.2006.02.007

     

    罗镇宽, 苗来成, 关康. 2000. 华北地台北缘金矿床成矿时代讨论. 黄金地质, 6(2): 70-76 https://www.cnki.com.cn/Article/CJFDTOTAL-HJDZ200002012.htm

     

    马寅生, 崔盛芹, 赵越, 曾庆利, 吴满路. 2002. 华北北部中新生代构造体制的转换过程. 地质力学学报, 8(1): 15-25 doi: 10.3969/j.issn.1006-6616.2002.01.002

     

    毛景文, 张作衡, 余金杰, 王义天, 牛宝贵. 2003. 华北及邻区中生代大规模成矿的地球动力学背景: 从金属矿床年龄精测得到启示. 中国科学(D辑), 33(4): 289-299 https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200304000.htm

     

    毛景文, 谢桂青, 张作衡, 李晓峰, 王义天, 张长青, 李永峰. 2005. 中国北方中生代大规模成矿作用的期次及其地球动力学背景. 岩石学报, 21(1): 169-188 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20050118&journal_id=ysxb

     

    邵济安, 何国琦, 唐克东. 2015. 华北北部二叠纪陆壳演化. 岩石学报, 31(1): 47-55 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20150103&journal_id=ysxb

     

    石来生, 饶玉学, 宋瑞先, 温建华. 2007. 河北省张家口金矿集区同位素及包裹体地质特征. 矿产与地质, 21(3): 219-227 doi: 10.3969/j.issn.1001-5663.2007.03.001

     

    宋国瑞, 赵振华. 1996. 河北省东坪碱性杂岩金矿地质. 北京: 地震出版社

     

    宋瑞先, 魏明辉, 王金锁等. 2013. 张家口地质矿产. 北京: 地质出版社

     

    孙金凤, 杨进辉. 2009. 华北东部早白垩世A型花岗岩与克拉通破坏. 地球科学(中国地质大学学报), 34(1): 137-147 https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200901015.htm

     

    陶利鑫, 甄世民, 白海军, 王江, 王大钊, 查钟健. 2020. 河北大白阳金矿床黄铁矿微量元素及S-Pb同位素地球化学特征. 吉林大学学报(地球科学版), 50(5): 1582-1598 https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ202005021.htm

     

    田伟, 陈斌, 刘超群, 张华峰. 2007. 冀北小张家口超基性岩体的锆石U-Pb年龄和Hf同位素组成. 岩石学报, 23(3): 583-590 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20070355&journal_id=ysxb

     

    王大钊, 刘家军, 翟德高, 甄世民, 王江. 2020. 河北东坪碲金矿床辉钼矿Re-Os及锆石U-Pb年龄研究. 地学前缘, 27(2): 405-419 https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202002026.htm

     

    王建平, 刘永山, 董法先, 李中坚, 彭华, 王连捷, 丁原辰, 杨玉东, 孟宪刚, 贾宏杰, 刘志斌, 刘建民, 王红才. 1992. 内蒙古金厂沟梁金矿构造控矿分析. 北京: 地质出版社

     

    王梁, 王根厚, 雷时斌, 常春郊, 侯万荣, 贾丽琼, 赵广明, 陈海舰. 2015. 内蒙武川后石花金矿床辉钼矿Re-Os同位素年龄及其地质意义. 地质与勘探, 51(3): 422-431 https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201503003.htm

     

    王时麟. 1986. 张家口金矿的成因研究. 北京大学学报(自然科学版), (4): 81-89 https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ198604011.htm

     

    王郁, 蒋心明, 王正坤. 1990. 河北省张-宣地区金矿床的硫、铅同位素地质研究. 地质找矿论丛, 5(2): 66-75 https://www.cnki.com.cn/Article/CJFDTOTAL-DZZK199002009.htm

     

    王正坤, 蒋心明, 王郁, 商木元. 1992. 张宣地区小营盘、东坪金矿的地质地球化学对比. 地质与勘探, (7): 14-20 https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT199207002.htm

     

    韦忠良, 张宏, 柳小明, 张晔卿. 2008. 张家口地区张家口组火山岩的LA-ICP-MS测年及其地质意义. 自然科学进展, 18(5): 523-530 doi: 10.3321/j.issn:1002-008X.2008.05.006

     

    吴福元, 徐义刚, 高山, 郑建平, 2008. 华北岩石圈减薄与克拉通破坏研究的主要学术争论. 岩石学报. 24(6): 1145-1174 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20080601&journal_id=ysxb

     

    吴福元, 刘小驰, 纪伟强, 王佳敏, 杨雷. 2017. 高分异花岗岩的识别与研究. 中国科学(地球科学), 47(7): 745-765 https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201707001.htm

     

    吴姗姗. 2009. 河北崇礼中山沟金矿成矿控矿构造研究. 硕士学位论文. 石家庄: 石家庄经济学院

     

    杨进辉, 吴福元, 柳小明, 谢烈文. 2005. 北京密云环斑花岗岩锆石U-Pb年龄和Hf同位素及其地质意义. 岩石学报, 21(6): 1633-1644 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=200506167&journal_id=ysxb

     

    杨进辉, 吴福元, 邵济安, 谢烈文, 柳小明. 2006. 冀北张-宣地区后城组、张家口组火山岩锆石U-Pb年龄和Hf同位素. 地球科学(中国地质大学学报), 31(1): 71-80 https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200601011.htm

     

    银剑钊, 史红云. 1995. 张家口-宣化地区金矿地质. 北京: 地质出版社

     

    曾庆栋, 刘建明, 张作伦, 覃锋, 陈伟军, 张瑞斌, 于昌明, 叶杰. 2009. 华北克拉通北缘鸡冠山斑岩钼矿床成矿年代及印支期成矿事件. 岩石学报, 25(2): 393-398 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20090213&journal_id=ysxb

     

    翟明国, 彭澎, 2007. 华北克拉通古元古代构造事件. 岩石学报, 23(11): 2665-2682 doi: 10.3969/j.issn.1000-0569.2007.11.001 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=200701101&journal_id=ysxb

     

    翟明国. 2010. 华北克拉通的形成演化与成矿作用. 矿床地质, 29(1): 24-36 doi: 10.3969/j.issn.0258-7106.2010.01.004

     

    张超, 马昌前, Holtz F. 2012. 含水大陆下地壳的部分熔融: 大别山C型埃达克岩成因探讨. 高校地质学报, 18(1): 41-51 doi: 10.3969/j.issn.1006-7493.2012.01.004

     

    张超, 郭巍, 徐仲元, 刘正宏, 刘永江, 雷聪聪. 2014. 吉林东部延边地区二长花岗岩年代学、岩石成因学及其构造意义研究. 岩石学报, 30(2): 512-526 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20140215&journal_id=ysxb

     

    张莉莉, 江思宏, 李红梅, 吴迪, 康欢. 2019. 河北丰宁撒岱沟门钼矿床成岩成矿年代学及成矿岩体地球化学特征. 地球学报, 40(5): 708-724 https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201905005.htm

     

    张彤, 陈志勇, 许立权, 陈郑辉. 2009. 内蒙古卓资县大苏计钼矿辉钼矿铼-锇同位素定年及其地质意义. 岩矿测试, 28(3): 279-282 doi: 10.3969/j.issn.0254-5357.2009.03.017

     

    张晓晖, 翟明国. 2010. 华北北部古生代大陆地壳增生过程中的岩浆作用与成矿效应. 岩石学报, 26(5): 1329-1341 http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?flag=1&file_no=20100501&journal_id=ysxb

     

    张招崇. 1995. 冀北水泉沟杂岩体的成因机制及其与金的成矿作用关系的研究. 博士学位论文. 北京: 中国地质科学院

     

    张招崇, 陈洪新, 1997. 水泉沟杂岩体的地质学和岩石学研究. 贵金属地质, 6(2): 81-92 https://www.cnki.com.cn/Article/CJFDTOTAL-GJSD702.000.htm

     

    赵越, 翟明国, 陈虹, 张拴宏. 2017. 华北克拉通及相邻造山带古生代-侏罗纪早期大地构造演化. 中国地质, 44(1): 44-60 doi: 10.3969/j.issn.1672-6995.2017.01.011

     

    甄世民, 查钟健, 王大钊, 刘家军, 庞振山, 程志中, 薛建玲, 王江, 白海军, 李阳, 陈超. 2021. 河北张宣地区中山沟金矿成矿流体特征及其对侵入岩型碲金矿床的限定. 中国地质: 1-27

  • 加载中

(15)

(3)

计量
  • 文章访问数: 
  • PDF下载数: 
  • 施引文献:  0
出版历程
收稿日期:  2021-01-01
修回日期:  2021-04-14
刊出日期:  2021-06-01

目录