Active subduction and strain partitioning in western Myanmar revealed by a dense survey GNSS network
The active tectonics of the Myanmar (formerly Burma) microplate in central Myanmar are caused by the oblique collision between the Sunda and Eurasia plates to the east and the Indian plate to the west. The kinematics of this plate boundary zone remain a subject of controversy, due in part to limited...
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Main Authors: | , , , , , , , , , , , , , , , , |
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格式: | Article |
語言: | English |
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2024
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在線閱讀: | https://hdl.handle.net/10356/174343 |
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機構: | Nanyang Technological University |
語言: | English |