碩士 / 國立臺灣大學 / 海洋研究所 / 104 / Taiwan is at the boundary between the Eurasian Plate and the Philippine Sea Plate, and the Philippine Sea Plate is moving northwest toward the Eurasia Plate at a rate of ~72 mm/yr. The collision between them resulting in Taiwan orogeny, and forming a fold-and-thrust belt aglined in nouth-south direction. Therefore, the western plains and foothills of Taiwan have formed by the action of the north-south strike reverse faults in the belt. More to the west, the age of fault is younger , and the dip is smaller. These structure lines will extend south to Kaoping area. Most geologists believe that the youngest Changhua fault extends southly to Tainan area, but becomes fragmented further to south; therefore, fault line is hard to located especially in Tainan area. According to the reflection seismic profiles, in the continental slope offshore the Tainan and Kaohsiung areas, some researchers believe the paleo-trace of the Manila Trench can be extending northwards and connected to the Changhua fault, marking a deformation front going from land to ocean floor. However, their conclusions lack nearshore topographical and geophysical data such that the doublt has been prevailed to support the Manila Trench was previously located in Taiwan Orogon. Therefore, nearshore geophysical survey was conducted off Tainan coast, firstly, the R2 Multi-beam Sounder was used and the significant topographical lineations related with those geological structures shown onland Tainan are found. Besides, by using 3.5 kHz bottom profiler, the dislocation in shallow sediments is also dominant. This study indicates there is less evidence to suggest the deformation front formed along Taiwan Isand can extends offshore into the continental slope and shall connect with the Manila Trench. We suggest that these topography and shallow structure are the extension of Hsinhua fault and Houchiali Fault. When they extend to the study area , they convert into a right lateral fault which affect by several extensional normal faults, these normal faults are called listric fault. Listric fault often arranged in house-tail. The end of the fault torn into a extensional basin.
| Identifer | oai:union.ndltd.org:TW/104NTU05279013 |
| Date | January 2016 |
| Creators | Cheng-Wei Hsieh, 謝正緯 |
| Contributors | 宋國士 |
| Source Sets | National Digital Library of Theses and Dissertations in Taiwan |
| Language | zh-TW |
| Detected Language | English |
| Type | 學位論文 ; thesis |
| Format | 85 |
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