Millennial slip rate of the Longitudinal Valley fault from river terraces : implications for convergence across the active suture of eastern Taiwan
The Longitudinal Valley fault is a key element in the active tectonics of Taiwan. It is the principal structure accommodating convergence across one of the two active sutures of the Taiwan orogeny. To understand more precisely its role in the suturing process, we analyzed fluvial terraces along the...
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Main Authors: | , , , , |
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格式: | Article |
語言: | English |
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2012
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在線閱讀: | https://hdl.handle.net/10356/95555 http://hdl.handle.net/10220/8478 |
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機構: | Nanyang Technological University |
語言: | English |