The mechanism of forearc basement subduction and frontal accretional cycle in southern Taiwan: Insights from sandbox modeling
碩士 === 國立臺灣大學 === 地質科學研究所 === 101 === The active Taiwan orogenic belt is considered as formed by the Eurasian plate obliquely converging with the Philippine Sea plate. In southern offshore of Taiwan, the oceanic lithosphere subducted eastward beneath the Philippine Sea Plate along the Manila Trenc...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2013
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| Online Access: | http://ndltd.ncl.edu.tw/handle/90388816853866983966 |