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DOI10.1002/gj.4735
Brittle failures and vein formation in the evolution of the South Qiangtang accretionary complex in the Tibetan Plateau
Li, Peng-Sheng; Li, Dian; Hu, Yi-Ling; Pei, Qiu-Ming; Wang, Gen-Hou; Zou, Hao; Liu, Zheng-Yong; Li, Yang; Guo, Jing; He, Ya-Dong
发表日期2023
ISSN0072-1050
EISSN1099-1034
起始页码3043
结束页码3062
卷号58期号:8
英文摘要The genesis of the subduction melange in the central Qiangtang terrane has been a long hot debate. However, little research has been conducted on the brittle failure within the accretionary wedge, which is very important to unveil the structural evolution of the melange. In this study, based on the recognition of multiple deformational phases, we analyse the characteristics and formation history of the vein system in the Gangma Co melange. Six groups of quartz veins are recognized. Foliation-parallel extension veins (G1 veins), shear veins (G2 veins) and foliation-perpendicular extension veins (G4 veins) are supposed to have formed during the subduction of oceanic crust, recording the repeated low-angle thrust-sense frictional sliding, tensile fracturing and stress changes generated by subduction-related earthquakes. Subsequent vertical extension veins (G5 veins) are suggested to be related to the exhumation of the underplated melange, while the horizontal extension veins (G6 veins) in the last phase represent the final horizontal thrusting. The temperature conditions for shear vein formation were examined by fluid inclusion analysis, ranging from 120 to 200 degrees C, coinciding with the temperature conditions of the slow earthquake region where episodic tremors and slow slip occur. This contribution supports that the Gangma Co melange represents an in situ subduction zone and that its internal vein system is a response to the tectonic evolution of the Longmu Co-Shuanghu Tethys Ocean.
关键词brittle failuremelangeQiangtang terranequartz veinsTibetan Plateau
英文关键词NORTHERN TIBET; SUBDUCTION-ZONE; METAMORPHIC BELT; INTRAOCEANIC ARC; LHASA TERRANE; SHEAR ZONE; FLUID-FLOW; SLOW SLIP; STRESS; PROVENANCE
WOS研究方向Geosciences, Multidisciplinary
WOS记录号WOS:000959902700001
来源期刊GEOLOGICAL JOURNAL
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/283873
作者单位Chengdu University of Technology; Southwest Jiaotong University; China University of Geosciences - Beijing; Chengdu University of Technology; Southwest Jiaotong University
推荐引用方式
GB/T 7714
Li, Peng-Sheng,Li, Dian,Hu, Yi-Ling,et al. Brittle failures and vein formation in the evolution of the South Qiangtang accretionary complex in the Tibetan Plateau[J],2023,58(8).
APA Li, Peng-Sheng.,Li, Dian.,Hu, Yi-Ling.,Pei, Qiu-Ming.,Wang, Gen-Hou.,...&He, Ya-Dong.(2023).Brittle failures and vein formation in the evolution of the South Qiangtang accretionary complex in the Tibetan Plateau.GEOLOGICAL JOURNAL,58(8).
MLA Li, Peng-Sheng,et al."Brittle failures and vein formation in the evolution of the South Qiangtang accretionary complex in the Tibetan Plateau".GEOLOGICAL JOURNAL 58.8(2023).
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