收稿日期: 2019-01-14
修回日期: 2019-04-10
网络出版日期: 2019-07-05
基金资助
国家自然科学基金项目“2015年尼泊尔地震相关地质灾害的地震学成因”（编号：41761144076）和“第二次青藏高原综合科学考察研究”(2019QZKK0701)
Seismic Activity in the Himalayan Orogenic Belt and Its Related Geohazards
Received date: 2019-01-14
Revised date: 2019-04-10
Online published: 2019-07-05
Supported by
Foundation item: Project supported by the National Natural Science Foundation of China “The seismic control of geohazards related to the 2015 Nepal earthquake” (No. 41761144076) and "the 2nd Scientific Expedition to the Qinghai-Tibet Plateau"(No. 2019QZKK0701)
喜马拉雅造山带是地球上海拔最高、规模最大的陆陆板块俯冲碰撞带。在这条长达2 500 km的板块边界上，近年来多次发生破坏性地震，造成大规模的滑坡、房屋倒塌等次生灾害，给人民生命和财产安全造成严重的威胁。分别选取尼泊尔喜马拉雅、喜马拉雅东构造结和喜马拉雅西构造结地区近期发生的3个地震震群作为研究实例，基于中国科学院青藏高原研究所在研究区架设的区域流动地震台站记录的波形资料，对地震的震源位置和震源机制解进行计算。结果表明，在尼泊尔喜马拉雅地区，主喜马拉雅逆冲断裂是大地震的主要发震构造；东构造结地区的地震以逆冲和走滑型为主，表明印度板块向北东方向的逆冲推覆和青藏高原向东南逃逸的侧向挤出是该地区的主要构造背景；西构造结地区中深源地震多发，揭示了高角度大陆深俯冲的几何形态。
白玲 , 宋博文 , 李国辉 , 江勇 . 喜马拉雅造山带地震活动及其相关地质灾害[J]. 地球科学进展, 2019 , 34(6) : 629 -639 . DOI: 10.11867/j.issn.1001-8166.2019.06.0629
Himalayan orogenic belt is the highest and largest continental collision and subduction zone on the Earth. The Himalayan orogenic belt has produced frequent large earthquakes and caused several geohazards due to landslides and housing collapse, having an impact on the safety of life and property along a length of over 2500 km. Here we took three earthquake clusters as examples, which occurred at Nepal Himalaya, eastern Himalayan syntaxis and western Himalayan syntaxis, respectively. Here we calculated the earthquake locations and fault plane solutions based on the waveform data recorded by seismic stations deployed in source areas by the Institute of Tibetan Plateau Research, Chinese Academy of Sciences. We found that at the Nepal Himalayan, the Main Himalayan Thrust is the major tectonic structure for large earthquakes to occur. At the eastern Himalayan syntaxis, most earthquakes are of the reverse or strike-slip faulting. The major tectonic feature is the combination of the NE-dipping thrust with the southeastern escape of the Tibetan plateau. At the western Himalayan syntaxis, intermediate-depth earthquakes are active. These observations reveal the geometry of the deep subduction of the continental plate with steep dipping angle.
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