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Taiwan Academic Institutional Repository >
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"yu ho shing"
Showing items 1-10 of 56 (6 Page(s) Totally) 1 2 3 4 5 6 > >> View [10|25|50] records per page
| 國立臺灣大學 |
2009 |
Morphotectonics and sedimentation in convergent margin basins: An example from juxtaposed marginal sea basin and foreland basin, Northern South China Sea
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Yu, Ho-Shing; Huang, Zehn-Yin |
| 國立臺灣大學 |
2009 |
Tectonically active sediment dispersal system in SW Taiwan margin with emphasis on the Gaoping (Kaoping) Submarine Canyon
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Yu, Ho-Shing; Chiang, Cheng-Shing; Shen, Su-Min |
| 國立臺灣大學 |
2009 |
Links among slope morphology, canyon types and tectonics on passive and active margins in the northernmost South China Sea
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Yu, Ho-Shing; Chang, Emmy T. Y. |
| 臺大學術典藏 |
2009 |
Tectonically active sediment dispersal system in SW Taiwan margin with emphasis on the Gaoping (Kaoping) Submarine Canyon
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Shen, Su-Min; Chiang, Cheng-Shing; Yu, Ho-Shing; Chiang, Cheng-Shing; Shen, Su-Min; Yu, Ho-Shing |
| 國立臺灣大學 |
2008 |
Morphology and sedimentation of sand bodies in the tidal shelf sea of eastern Taiwan Strait
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Liao, Horn-Ru; Yu, Ho-Shing; Su, Chih-Chieh |
| 國立臺灣大學 |
2008 |
Evidence of hyperpycnal flows at the head of the meandering Kaoping Canyon off SW Taiwan
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Chiang, Cheng-Shing; Yu, Ho-Shing |
| 國立臺灣大學 |
2006 |
Intraslope Basin, Seismic Facies and Sedimentary Processes in the Kaoping Slope, Offshore Southwestern Taiwan
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Yu, Ho-Shing; Huang, Zehn-Yin |
| 國立臺灣大學 |
2006 |
Shifting submarine canyons and development of a foreland basin in SW Taiwan: controls of foreland sedimentation and longitudinal sediment transport
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Yu, Ho-Shing; Hong, Eason |
| 國立臺灣大學 |
2006 |
Morphotectonics and incision of the Kaoping submarine canyon, SW Taiwan orogenic wedge
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Chiang, Cheng-Shing; Yu, Ho-Shing |
| 國立臺灣大學 |
2006 |
GPR reflection characteristics and depositional models of mud volcanic sediments—Wushanting mud volcano field, southwestern Taiwan
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Chow, Joseph Jinder; Chang, Su-Kai; Yu, Ho-Shing |
Showing items 1-10 of 56 (6 Page(s) Totally) 1 2 3 4 5 6 > >> View [10|25|50] records per page
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