Slab models beneath central Myanmar revealed by a joint inversion of regional and teleseismic traveltime data

The intermediate-depth (50–180 km) seismicity beneath Myanmar provides direct evidence of the subducting Indian slab. However, the historic lack of regional seismic observations leads to previous low-resolution models that show large variations in slab geometry beneath Myanmar. The depth extent and...

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Bibliographic Details
Main Authors: Yao, Jiayuan, Liu, Shaolin, Wei, Shengji, Hubbard, Judith, Huang, Bor-Shouh, Chen, Meng, Tong, Ping
Other Authors: School of Physical and Mathematical Sciences
Format: Article
Language:English
Published: 2021
Subjects:
Online Access:https://hdl.handle.net/10356/151810
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Institution: Nanyang Technological University
Language: English