Facies Analysis and Depositional History of the Taipei Basin
碩士 === 國立臺灣大學 === 地質科學研究所 === 106 === In the northern tip of the active Taiwan Mountain Belt, a Quaternary extensional basin, namely Taipei Basin, has developed atop the deformed orogenic basement as a result of post-orogenic collapse, and comprises 670m siliciclastic sediments infill. This study pr...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2018
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| Online Access: | http://ndltd.ncl.edu.tw/handle/nhu7p4 |