龙岗火山群第四纪爆破式火山作用类型与期次研究
Study on type and phase of Quaternary explosive volcanism in Longgang volcanic duster.
-
摘要: 龙岗火山群位于吉林省辉南和靖宇县境内的龙岗山脉中段。火山活动始于新近纪,第四纪更新世为鼎盛期,全新世以来仍有较强的喷发活动,是中国近代活动火山区之一。火山碎屑物的堆积构造、组成、显微形貌和粒度特征表明,第四纪爆破式火山作用包括岩浆爆发、射汽一岩浆爆发和射汽爆发三种类型,以岩浆和射汽-岩浆爆发最为发育。区内爆破式火山活动具有多旋回、多期次、多阶段喷发特点。据火山地质特征,可划分为9期,由老至新为:早更新世早期、晚期;中更新世三角龙湾期、旱龙湾期和金龙顶子早期;晚更新世金川东期;全新世大翁圈期、红期林场期和金龙顶子晚期。爆破式火山灾害的范围较大,岩浆爆发中高危区的半径约10km。射汽-岩浆爆发影响的半径约4km。Abstract: Longgang volcanic cluster is located in Huinan and Jingyu counties and belongs to the middle segment of the Longgang mountains range. Volcanic activities began in Neogene, and gained the prime of its life in Quarternary. Relative strong eruptions still occurred since Holocene. The features of depositional structure, components, micromorphology and grain size of pyroclastic materials show that the Quaternary explosive activities involve magmatic explosions, phreatomagmatic explosions and phreatic explosions. Magmatic explosions, phreatomagmatic explosions have the highest magnitude. Multi-cycle, multi-episode and multi-stages characterize the explosive activity of this cluster together. The Quaternary explosions can be divided into 9 stages according to the volcano-geological features. The hazard coverage of explosive volcanoes is great. The radius of middlehigh hazardous area resulted from a magmatic explosion is about 10km, while the radius involved in a phreatomagmatic explosion is about 4km.
-
Key words:
- Longgang volcanic cluster /
- Explosive volcanism /
- Type /
- Phase
-
-
[1] Bureau of geology and mineral resources Jilin.1982. Regional Geology of Jinlin Province.Beijing:Geological Publishing House:270-272(in Chinese)
[2] Cas R A F,Wright J V.1987. Volcanic succession-modern and ancient.London:UNWIN HYMAN,10-328
[3] Eduardo P,Hector C.1990. Volcanic hazard maps of the Nevado del Ruiz Volcano colmbia.Amsterdam.J.Volcanol.Geotherm.Res,42:117-127
[4] Fan Q C,Hooper P R.1991. The Cenozoic basaltic rocks of eastern China:petrology and chemical composition.Journal of petrology,32(4):765 -810
[5] Fan Qicheng,Sui Jianli,Liu Ruoxin,el al.2002. Periods of Quaternary volcanic in Longgang area,Jilin Province.Acta Petrologic Sinica,18(4):495 -500 (in Chinese with English abstract)
[6] Liu Jiaqi,1988. The cenozoic volcanic episodes in Northeast China.Acta Petrologica Sinica,(1):1 -10 (in Chinese with English abstract)
[7] Liu Jiaqi,1995. Volcanism and its potential hazards in China.In:Liu Ruoxin,ed.Volcanism and man\'s environment.Beijing:Earthquake Press:182 -190 (in Chinese)
[8] Liu Jiaqi,1999. Volcanoes in China.Beijing:Science Press:1-125 (in Chinese)
[9] Liu Jiaqi.1987. Studies on the geochronology of the Cenozoic volcanic rocks in Northeastern China.Acta Petrologica Sinica,(4):21-31(in Chinese with English abstract)
[10] Liu Ruoxin,ed.2000. Active volcanoes in China.Beijing:Earthquake Press:67-74 (in Chinese)
[11] Liu Xiang,Wang Xikui.1987. Discovery of base-surge in the Dalongwan of Huinan County,Jilin Province.Geological Review.33 (6):577-582 (in Chinese with English abstract)
[12] Liu Xiang,Xiang Tianyuan.1997. Cenozoic volcanoes and pyroclastic deposits in Northeastern China resources and hazards.Changchun:Jilin University Publishing House:83 -106,142 (in Chinese)
[13] Liu xiang,Xiang Tianyuan,Wang Xikui.1989. Episodes of cenozoic volcanism in the Changbai mountains area.Geological Jilin,(1):30-41 (in Chinese with English abstract)
[14] Sui Jianli,Fan Qicheng,Cao Jie.1999. A preliminary study of eruption features and petrochemistry of volcanic rocks from the Longgang volcanoes.Geological Review.45 (sup):319-324 (in Chinese with English abstract)
[15] Wang Yansheng,Jin Ke.1999. Division and eruption types of the cenozoic Longgang Volcano Cluster,Jilin Province.Geoloical Review.45(sup):332 -337 (in Chinese with English abstract)
[16] Wang Yujun,Sun Jianzhong.1980. Episodes of cenozoic volcanism in Jilin Province.Geological Jilin,(3):6-251 (in Chinese)
[17] Wei Haiquan,Liu Ruoxin,Fan Qicheng,el al.1999. Monogenetic volcanism in Longgang Volcano Clusters.Geological Review.45(sup):325 -331 (in Chinese with English abstract)
[18] Wohletz K H,Sheridan M F.1983. Hydrovolcanic explosions Ⅱ.Evolution of tuff rings and tuff cones.Am.J.Sci,283:385 -413
[19] Xu Debiu,Bai Zhida,Zhang Bingliang,el al.2005. Characteristic and genetic mechanism of pyrclastic base-surge deposits of volcanic swarm in Longgang Area,Jilin Province.Acta Sedimentologica Sinica,23 (1):60 -66 (in Chinese with English abstract)
[20] 樊祺诚,隋建立,刘若新等.2002.吉林龙岗第四纪火山活动分期.岩石学报,18(4):495-500
[21] 吉林省地质矿产局.1982.吉林省区域地质志.北京:地质出版社:270-272
[22] 刘嘉麒.1987.中国东北地区新生代火山岩的年代学研究.岩石学报,(4):21-31
[23] 刘嘉麒.1988.中国东北地区新生代火山幕.岩石学报,(1):1-10
[24] 刘嘉麒.1995.中国火山活动及其潜在的危险.见:刘若新主编,火山作用与人类环境.北京:地震出版社:182-190
[25] 刘嘉麒.1999.中国火山.北京:科学出版社:1-125
[26] 刘若新.2000.中国的活火山.北京:地震出版社:67-74
[27] 刘祥,王锡魁.1987.吉林省辉南县大龙湾火山基浪(base-surge)堆积物的发现.地质论评,33(6):577-582
[28] 刘祥,向天元,王锡魁1989.长白山地区新生代火山活动分期,吉林地质,(1):30-41
[29] 刘祥,向天元.1997中国东北地区新生代火山和火山碎屑堆积物资源与灾害.长春:吉林大学出版社:83-106,142
[30] 隋建立,樊祺成,曹杰.1999.龙岗火山喷发特征与火山岩化学初步研究.地质论评,45(sup):319-324
[31] 王彦生,靳克.1999.吉林省新生代龙岗火山群期次划分及火山喷发类型特点.地质论评,45(sup):332-337
[32] 王雨鈞,孙建中.1980.吉林省新生代火山活动期次初步划分.吉林地质,(3):6-25
[33] 魏海全,刘若新,樊祺诚等.1999.龙岗火山群单成因火山作用.地质论评,45(sup):325-331
[34] 徐德兵,白志达,张秉良等.2005,吉林龙岗火山群火山碎屑基浪堆积特征与成因机理.沉积学报,23(1):60-66
-
计量
- 文章访问数:
- PDF下载数:
- 施引文献: 0