The thermal history of the Shuilien Conglomerate in the coastal range, Eastern Taiwan and their implications
碩士 === 國立東華大學 === 地球科學研究所 === 98 === Taiwan orogen was formed by oblique collision of Luzon arc against the Eurasian continent. The thermal history of the orogen was recorded in the eroded materials from the overgrown accretionary prism. Carbonaceous materials (CM) are not sensitive to the retrograd...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2010
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| Online Access: | http://ndltd.ncl.edu.tw/handle/86940382913382026536 |