P-Wave Velocity Structures of the Crust across Southern Taiwan Strait Analyzed by Using Ocean-Bottom Seismometers
碩士 === 國立臺灣海洋大學 === 應用地球科學研究所 === 104 === Extension in Taiwan Strait was caused by flexural bending of the Eurasian Plate in response to the load of Taiwan orogenic belt. Mega earthquakes, such as Quanzhou Earthquake (Mw~8.0) in 1604, Nanao Earthquake (Mw~7 and Mw~7.5) in 1600 and 1918, Taiwan S...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2016
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| Online Access: | http://ndltd.ncl.edu.tw/handle/wfvep9 |