东天山地区两类钒钛磁铁矿型矿床含矿岩石对比

王玉往[1,2,3] 王京彬[1,2,3] 王莉娟[2,3]. 东天山地区两类钒钛磁铁矿型矿床含矿岩石对比[J]. 岩石学报, 2006, 22(5): 1425-1436.
引用本文: 王玉往[1,2,3] 王京彬[1,2,3] 王莉娟[2,3]. 东天山地区两类钒钛磁铁矿型矿床含矿岩石对比[J]. 岩石学报, 2006, 22(5): 1425-1436.
WANG YuWang, WANG JingBin and WANG LiJuan. Comparison of host rocks between two vanadic titianomagnetite deposit types from the eastern Tianshan mountains.[J]. Acta Petrologica Sinica, 2006, 22(5): 1425-1436.
Citation: WANG YuWang, WANG JingBin and WANG LiJuan. Comparison of host rocks between two vanadic titianomagnetite deposit types from the eastern Tianshan mountains.[J]. Acta Petrologica Sinica, 2006, 22(5): 1425-1436.

东天山地区两类钒钛磁铁矿型矿床含矿岩石对比

  • 基金项目:

    本文由国家重点基础研究项目(编号:2001CB409806)资助.致谢 野外工作中得到新疆有色地质四队领导和同志们大力支持,成文过程中得到顾连兴老师认真负责的审阅和修改,在此深表感谢!

Comparison of host rocks between two vanadic titianomagnetite deposit types from the eastern Tianshan mountains.

  • 新疆东天山地区产出有两类岩浆型钒钛磁铁矿矿床,分别以尾亚和香山西矿床为代表。尾亚是以铁钛为主的中型钒钛磁铁矿矿床,香山西则是以钛为主的大型钛铁矿矿床,与铜镍矿床共生。尾亚矿床含矿岩石的岩石学、岩石化学、稀土及微量元素特征与典型的钒钛磁铁矿矿床相似。而香山西矿床含矿岩石的碱度、镁铁指数(FeO^*/MgO)、岩浆酸度(αsi)、钙碱富集指数(calk/m)等地球化学参数,氧逸度和硫逸度等物理化学参数均介于独立的典型铜镍硫化物和典型钒钛磁铁矿矿床之间。两类矿床含矿岩石特征的差异可能在于其产出的构造背景不同,导致其含矿岩浆演化过程中处于不同的物理化学条件。
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  • [1]

    Feng Yimin,Zhu Baoqing,Yang Junlu,et al.2002. Tectonics and evolution of the eastern Tianshan mountains-a brief introduction to "tectonic map (1:500000) of the eastern Tianshan Mountains of Xinjiang.Xinjiang Geology,20(4):309 -314

    [2]

    Fleet M.E.and MacBade.1983. Distribution coefficient of nickel between olivine and sulfide and its application on copper-nickel sulfide deposit.In:Institute of Geology for Mineral Resources,CNNC.Orthomagrnatic Cu-Ni-PGE Sulfide Deposit.1988.171 -179 (unpublished data,in Chinese)

    [3]

    Fleet M.E.,Chryssoulis S.L.,and Stone W.E.1993. Partitioning of platinum-group elements and Au in the Fe-Ni-Cu-S system:experiments on the fractional crystallization of sulfide melt.Contributions to Mineralogy and Petrology,115:36 -34

    [4]

    Frost D.J.and Wood B.J.1997. Experimental measurements of the oxygen fugacity of CO2 and graphite/diamond stability from 35 to 77kbar at 925 to 1650℃.Geochim.Cosmochim.Acta.,61:1565 -1574

    [5]

    Fu Xueming and Liu Fengshan.1992. Ore-forming mechanism of Cu-Ni sulfide deposit-giving Huangshan Cu-Ni sulfide deposit near Hami city as an example.ACTA Geologica Gansu,1 (2):66-72 (in Chinese with English abstract)

    [6]

    Irvine T.N.and Baragar W.R.A.1971. A guide to the chemical classification of the common volcanic rocks.Can.,J.Earth Sci.,(8):523-548

    [7]

    Lai Shaocong.1994. Oxygen fugacity of magma affected by fractional crystallization.Earth Science Frontiers,1 (1 -2):12 (in Chinese)

    [8]

    Li Chengde,Mu Jilu,Zhu Guoqiang,et al.1996. Genesis and metallogenic Regularity of Shallow-Rich Orebody of Huangshan Metallogenic Belt Hami,Xinjiang.Chengdu:Chengdu Sci.& Tech.Univ.Press,1 -204 (in Chinese with English abstract)

    [9]

    Li C.,Naldrett A.J.and Ripley E.M.2001. Critical factors for the formation of a nickel-copper deposit in an evolved magma system:lessons from a comparison of the pants lake and Voisey\' s Bay sulfide occurrences in Labrador,Canada.Mineralium Deposita,36:85-92

    [10]

    Li Jinyi,Wang Kezhuo,Li Wenqian,et al.2002. Tectonic evolution since the Late Paleozoic and mineral prospecting in eastern Tianshan Mountains,NW China.Xinjiang Geology,20(4):295-302 (in Chinese with English abstract)

    [11]

    Li Jinyi.2004. Late Neoprotrozote and Paleozoic tectonic framework and evolution of eastern Xinjiang,NW China.Geological Review,50(3):304 -322 (in Chinese with English abstract)

    [12]

    Li Jinyi,He Guoqi,Xu Xin,et al.2006. Crustal tectonic framework of northern Xinjiang and adjacent regions and its formation.Acta Geologica Sinica,80 (1):148-168 (in Chinese with English abstract)

    [13]

    Li Quan,Yu Haifeng and Xiu Qunye.2002. On Precambrian basement of the eastern Tianshan Mountains,Xinjiang.Xinjiang Geology,20(4):346-351 (in Chinese with English abstract)

    [14]

    Li Songling and FengXinchang.1997. Super-unit association of Weiya,Eastern Tianshan of Xinjiang.Xinjiang Geology,15 (1):13-27(in Chinese with English abstract)

    [15]

    Liu Congqiang,Liheping,Huangzhilong,et al.2001. A review of studies on oxygen fugacity of the earth mantle.Earth Science Frontiers,8 (3):73-82 (in Chinese with English abstract)

    [16]

    Lu Jiren,Zhang Chengxin,Zhang Guangdi,et al.1988. Genetic type of V-Ti magnetite deposit in Panxhihua-Xichang area.Mineral Deposits,7 (1):1 -13 (in Chinese with English abstract)

    [17]

    Mei Houjun.1973. The relationship between the petrochemical characteristics of two trap series in southwestern China and related iron and nickel mineralizations.Geochemica,(4):219-253 (in Chinese with English abstract)

    [18]

    Naldrett A.J.1999. World-class Ni-Cu-PGE deposits:Key factors in their genesis.Mineralium Deposita,34:227 -240

    [19]

    Panxi Geological Party,Sichuan Bureau of Geology and Mineral Resources.1987. Metallogenetic Conditions and Geological Characteristics of the Hongge Vanadic Titianomagnetite Deposit,Sichuan.Beijing:Geological Publishing House,220pp (in Chinese with English abstract)

    [20]

    Qin Kezhang,Fang Tonghui,Wang Shulai,et al.2002. Plate tectonics division,evolution and metallogenic setting in eastern Tianshan Mountains,NW China.Xinjiang Geology,20(4):302-308 (in Chinese with English abstract)

    [21]

    Qin Quanxin.2003. Geological character of the ilmenite deposit in western part of Xiangshan and its genesis.Mineral Resources and Geology,17 (4):533 -535 (in Chinese with English abstract)

    [22]

    Qiu Jiaxiang and Lin Jingqian.1991. Petrochemistry.Beijing:Geological Publishing House,1 -276 (in Chinese)

    [23]

    Shimazaki H.and Naldrett A.J.1975. Solubility of sulfur in an ultramafic melt and relevance of the system Fe-S-O.Econ.Geol.,70:960-967

    [24]

    Thompson R.N.1982. Magmatism of the British Tertiary volcanic province.Scottish Journal of Geology.18(1):49-107

    [25]

    Vallace P.J and Gerlach T..M.1994. Magmatic vapor source for sulfur dioxide released during volcanic eruptions:evidence from Mount Pinatubo.Science,265:497-99

    [26]

    Wang Jingbin and Xuxin.2006. Post-collisional tectonic evolution and metallogenesis in northern Xinjiang,Chian.Acta Geologica Sinica,80(1):23 -31 (in Chinese with English abstract)

    [27]

    Wang Jingbin,WangG Yuwang and Wang Lijuan.2004. The Junggar immature continental crust province and its mineralization.Acta Geologica Sinica (English edition),78 (2):337-344

    [28]

    Wang Yuwang,Wang Jingbin,Wang Lijuan,et al.2004. REE characteristics of Cu-Ni sulfide deposits in the Huang area,Xinjiang.Acta Petrologica Sinica,20 (4):935-948 (in Chinese with English abstract)

    [29]

    Wang Yuwang,Wang Jingbin,Wang Lijuan,et al.2005. Weiya vanadium-bearing titianomagnetite deposit,Xinjiang-A polygenetic magmatic differentiation-magmatic injection-magmatic hydrothermal deposit.Mineral Deposits,24 (4):349-359 (in Chinese with English abstract)

    [30]

    Wang Yuwang,Wang Jingbin,Wang Lijuan,et al.2006. A intermediate type of Cu-Ni sulfide and V-Ti magnetite deposit:Xinjiang Xiangshanxi deposit,China.Acta Geologica Sinica,80(1):61 -73 (in Chinese with English abstract)

    [31]

    Will G.and Nover G.1979. Influence of oxygen partial pressure on the Mg/Fe distribution in olivine.Phys.Chem.Minerals,(4):199 -208

    [32]

    Wood D.A.1979. A variably veined suboceanic upper mantle-genetic significance for mid-ocean ridge basalts from geochemical evidence.Geology.7(10):499 -503

    [33]

    Xie Guanghong.1980. Petrochemical characteristics of the anorthosite suite in Damiao,Hebei province,China.Geochemica,(3):263 -277 (in Chinese with English abstract)

    [34]

    Xie Guanghong,Wang Yunliang,Fan Caiyun,et al.1998. Genetic mechanisms of the Jinchuan ultramafic intrusion and associated superlarge sulfide deposit,Northwest China.,Science in China (D),41 (Supp.):31 -36

    [35]

    Zhang Yunxiang,Luo Yaonan,Yang Chongxi,et al.1988. Panzhihiua-Xichang Rigt in China.Beijing:Geological Publishing house,325pp(in Chinese)

    [36]

    Zhang Zunzhong,Gu Lianxing,Wu Changzhi,et al.2005. Zircon SHRIMP dating for the Weiya pluton,eastern Tianshan:its geological implications.Acta Geologica Sinica (English edition),79(4):481 -490

    [37]

    冯益民,朱宝清,杨军录等.2002.东天山大地构造及演化--1:50万东天山大地构造图简要说明.新疆地质,20(4):309-314

    [38]

    Fleet M.E.和MacRade.1983.镍在橄榄石和硫化物之间的分配系数及其在铜镍硫化物矿床研究中的应用.见:中国有色工业总公司矿产地质研究院.岩浆铜-镍-铂硫化物矿床.1988.171-179.(内部资料)

    [39]

    傅学明,刘凤山.1992.硫化铜镍矿床成矿作用机理-以新疆哈密黄山硫化铜镍矿床为例.甘肃地质学报,1(2):66-72

    [40]

    赖绍聪.1994.分离结晶对岩浆氧逸度的影响.地学前缘,1(1-2):12

    [41]

    李承德,慕纪录,竺国强等.1996.新疆哈密黄山成矿带浅富矿成因与成矿规律.成都:成都科技大学出版社

    [42]

    李锦轶,王克卓,李文铅等.2002.东天山晚古生代以来大地构造与矿产勘查.新疆地质,20(4):295-301

    [43]

    李锦轶.2004.新疆东部新元古代晚期和古生代构造格局及其演变.地质论评,50(3):304-322

    [44]

    李锦轶,何国琦,徐新等.2006.新疆北部及邻区地壳构造格架及其形成过程的初步探讨.地质学报,80(1):148-168

    [45]

    李铨,于海峰,修群业.2002.东天山前寒武纪基底若干问题的讨论.新疆地质,20(4):346-351

    [46]

    李嵩龄,冯新昌.1997.新疆天山东部尾亚超单元组合特征.新疆地质,15(1):13-27

    [47]

    刘丛强,李和平,黄智龙等.2001.地幔氧逸度的研究进展.地学前缘,8(3):73-82

    [48]

    卢纪仁,张承信,张光第等.1988.攀西地区钒钛磁铁矿矿床的成因类型.矿床地质,7(1):1-13

    [49]

    梅厚钧.1973.西南暗色岩深渊分异两个系列的岩石化学特征与铁镍矿化的关系.地球化学,(4):219-253

    [50]

    秦克章,方同辉,王书来等.2002.东天山板块构造分区、演化与成矿地质背景研究.新疆地质,20(4):302-308

    [51]

    秦全新.2003.香山西段钛铁矿床地质特征及成因探讨.矿产与地质,17(4):533-535

    [52]

    邱家骧,林景仟.1991.岩石化学.北京:地质出版社,1-276

    [53]

    四川省地矿局攀西地质大队.1987.四川红格钒钛磁铁矿矿床成矿条件及地质特征.北京:地质出版社

    [54]

    王京彬,徐新.2006.新疆北部后碰撞构造演化与成矿.地质学报,80(1):23-31

    [55]

    王玉往,王京彬,王莉娟等.2004.新疆黄山地区铜镍硫化物矿床的稀土元素特征及意义.岩石学报,20(4):935-948

    [56]

    王玉往,王京彬,王莉娟等.2005.新疆尾亚钒钛磁铁矿--一个岩浆分异-贯入-热液型复成因矿床.矿床地质,24(4):349-359

    [57]

    王玉往,王京彬,王莉娟等.2006.岩浆铜镍矿与钒钛磁铁矿的过渡类型--新疆哈密香山西矿床.地质学报,80(1):61-73

    [58]

    解广轰.1980.大庙斜长岩杂岩体的岩石学特征.地球化学,(3):263-277

    [59]

    解广轰,汪云亮,范彩云等.1998.金川超镁铁岩侵入体及超大型硫化物矿床的成岩成矿机制.中国科学(D辑),28(增刊):31-36

    [60]

    张云湘,骆耀南,杨崇喜等.1988.攀西裂谷.北京:地质出版社

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出版历程
收稿日期:  2005-12-10
修回日期:  2006-04-22
刊出日期:  2006-05-31

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