Seismic imaging of the Main Frontal Thrust in Nepal reveals a shallow décollement and blind thrusting

Because great earthquakes in the Himalaya have an average recurrence interval exceeding 500 yr, most of what we know about past earthquakes comes from paleoseismology and tectonic geomorphology studies of the youngest fault system there, the Main Frontal Thrust (MFT). However, these data are sparse...

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Main Authors: Almeida, Rafael V., Hubbard, Judith, Liberty, Lee, Foster, Anna, Sapkota, Soma Nath
其他作者: Asian School of the Environment
格式: Article
語言:English
出版: 2019
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在線閱讀:https://hdl.handle.net/10356/88640
http://hdl.handle.net/10220/50459
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機構: Nanyang Technological University
語言: English