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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| Main Authors: | , , , , , , |
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| 格式: | Article |
| 語言: | English |
| 出版: |
2021
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| 在線閱讀: | https://hdl.handle.net/10356/151810 |
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