中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Palaeostress analysis using fault-slip data from the Xiangdong tungsten deposit in the central south China continent: Evolution of intraplate stress in the Middle Mesozoic

文献类型:期刊论文

作者Shan, Yehua1,3; Ni, Yongjin2; Liang, Xinquan1,3
刊名JOURNAL OF STRUCTURAL GEOLOGY
出版日期2023-05-01
卷号170页码:14
关键词Tungsten -bearing quartz veins Fault -slip data Palaeostress analysis South China continent Middle Mesozoic
ISSN号0191-8141
DOI10.1016/j.jsg.2023.104831
英文摘要In the central South China continent, the Xiangdong tungsten deposit associated with Late-Jurassic granitic intrusion offers an opportunity to examine the evolution of intraplate stress between the Late Jurassic and Early Cretaceous, which was a time of transition from regional shortening to regional extension. NE-ENE-striking, steeply-dipping, opening-mode tungsten-bearing quartz veins constitute the deposit. Favorable conditions for vein formation where densely spaced arrays have non-curving tips occur under remote stress with a large stress difference and hence in this case probably aligned with the horizontal maximum principal stress axis. Palaeo-stress analysis using fault-slip data measured on the side walls of underground mine levels yielded the optimal solution of two stresses characterized by an NNW-SSE-shortening strike-slip regime and an NNW-SSE exten-sional regime. Based on field observations, the first tectonic phase existed during meso-and epi-thermal mineralization, probably owing to the collision between the Siberia and Mongolia-Sino-Korean continents far to the north at the time, and the second tectonic phase appeared after hydrothermal mineralization, as a result of Cretaceous regional rifting. Therefore, multiple strike-slip deformations would have involved the study area during hypo-and epi-thermal mineralization in the Late Jurassic. This evidence does not support the mainstream extension model for Mesozoic tungsten mineralization in central South China.
WOS研究方向Geology
语种英语
WOS记录号WOS:000978339200001
源URL[http://ir.gig.ac.cn/handle/344008/74172]  
专题同位素地球化学国家重点实验室
通讯作者Shan, Yehua
作者单位1.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China
2.Shandong Earthquake Adm, Jinan 250021, Peoples R China
3.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
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GB/T 7714
Shan, Yehua,Ni, Yongjin,Liang, Xinquan. Palaeostress analysis using fault-slip data from the Xiangdong tungsten deposit in the central south China continent: Evolution of intraplate stress in the Middle Mesozoic[J]. JOURNAL OF STRUCTURAL GEOLOGY,2023,170:14.
APA Shan, Yehua,Ni, Yongjin,&Liang, Xinquan.(2023).Palaeostress analysis using fault-slip data from the Xiangdong tungsten deposit in the central south China continent: Evolution of intraplate stress in the Middle Mesozoic.JOURNAL OF STRUCTURAL GEOLOGY,170,14.
MLA Shan, Yehua,et al."Palaeostress analysis using fault-slip data from the Xiangdong tungsten deposit in the central south China continent: Evolution of intraplate stress in the Middle Mesozoic".JOURNAL OF STRUCTURAL GEOLOGY 170(2023):14.

入库方式: OAI收割

来源:广州地球化学研究所

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