Sediment Velocity Structures in the Taiwan Strait and the Coastal Plain of west Taiwan
碩士 === 國立中央大學 === 地球物理研究所 === 95 === The method of reflection seismic imaging displays subsurface structures in time rather than in depth. One therefore needs to know the 3-D distribution of subsurface velocity in order to convert seismic time into depth and obtain 3-D subsurface depth structures. I...
| 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/05196469270688784417 |