古地震学证据表明,主要的喜马拉雅推力在达吉林-锡金喜马拉雅山脉的细分

Atul Brice1,2, R Jayangondaperumal3, Rao Singh Priyanka4

  • 1Wadia Institute of Himalayan Geology, Dehradun, Uttarakhand, India.

Scientific reports
|June 24, 2024
PubMed
概括

达吉林-锡金喜马拉雅 (DSH) 部分的主要喜马拉雅推力可能不会主办大,连续的断裂. 古地震学数据显示,一个明显的150公里段,具有很长的复发间隔.

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