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
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.
科学领域:
- 地质物理学 地质物理学
- 古代地震学 (paleoseismology) 是一种古地震学.
- 构造学 构造学 构造学 构造学
背景情况:
- 主喜马拉雅推力对于长时间的表面破裂事件的能力是有争议的.
- 之前的研究表明,达吉林 - 锡金喜马拉雅山脉 (DSH) 中世纪的地震延长了700公里的破裂.
- 关于大喜马拉雅地震在DSH的破裂程度存在差异.
研究的目的:
- 为了调查 DSH 中的主要喜马拉雅推力的破裂行为.
- 解决古地震记录和地震断裂范围的差异.
- 确定 DSH 中地震事件的断段长度和复发间隔.
主要方法:
- 在Chenga村的一个断层的古地震学调查,DSH.
- 对地平面图层的分析和表面断层事件的约会.
- 对边界结构进行地质评估,以确定段边界.
主要成果:
- 在DSH中确定了一个表面断层事件,可追溯到公元前1313-395年.
- 建议DSH作为一个150公里独立的段落,由地质结构划界.
- 该部分的复发间隔估计为949-1963年.
结论:
- 该DSH作为一个独立的地震段,不参与>700公里的破裂.
- 长时间的复发间隔表明,在这个段内,地震事件很少发生,但可能很大.
- 这些发现挑战了DSH古地震事件与尼泊尔和不丹之前的相关性.
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