Study of an unconformity boundary between the Liuchungchi and Kanhsialiao Formations, southeastern Taiwan
碩士 === 國立臺灣大學 === 地質科學研究所 === 95 === The Penglai orogeny is forming a foreland basin in the southwestern Taiwan since the Pliocene. Because the foreland basin was a highly subsidence, that it was deposited a hugely Plio-Pleistocene sediments. Since the Plio-Pleistocene, the global sea-level changes...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2007
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| Online Access: | http://ndltd.ncl.edu.tw/handle/23207158213867656506 |