C
Char-Shine Liu
Researcher at National Taiwan University
Publications - 171
Citations - 6942
Char-Shine Liu is an academic researcher from National Taiwan University. The author has contributed to research in topics: Accretionary wedge & Subduction. The author has an hindex of 46, co-authored 159 publications receiving 6147 citations. Previous affiliations of Char-Shine Liu include Adept Technology & University of California, San Diego.
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Journal ArticleDOI
Okinawa trough backarc basin: Early tectonic and magmatic evolution
Jean-Claude Sibuet,Benoã®T. Deffontaines,Shu Kun Hsu,Nicolas Thareau,Jean-Pierre Le Formal,Char-Shine Liu +5 more
TL;DR: In this article, the direction of extension in the southwestern Okinawa Trough has been deduced from a comparison with analog modeling: the direction is N 150 o for the Pleistocene phase of extension (2-01 Ma) and N 170 O for the late Pleistian-Holocene phase (01-0 Ma) by comparing the two last extensional phases.
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Neotectonic architecture of Taiwan and its implications for future large earthquakes
TL;DR: In this article, the authors presented a neotectonic map of Taiwan based on structural and geomorphic expression of active faults and folds both in the field and on shaded relief maps prepared from a 40m resolution digital elevation model, augmented by geodetic and seismologic data.
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Feeding methane vents and gas hydrate deposits at south Hydrate Ridge
Anne M. Tréhu,Peter B. Flemings,Nathan L. Bangs,Johanna Chevallier,Eulàlia Gràcia,Joel E. Johnson,Char-Shine Liu,Xiaoli Liu,Michael Riedel,Marta E Torres +9 more
TL;DR: In this article, a coarse-grained turbidite sequence of the Cascadia accretionary complex is shown to have gas saturation as high as 90% in a coarse grained sequence.
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Provenance, structure, and formation of the mud wedge along inner continental shelf of the East China Sea: A synthesis of the Yangtze dispersal system
Kehui Xu,Anchun Li,J. Paul Liu,John D. Milliman,Zuosheng Yang,Char-Shine Liu,Shuh-Ji Kao,Shiming Wan,Fangjian Xu +8 more
TL;DR: In this article, the authors show that sediment along the innermost part of the continental shelf in East China Sea is mainly derived from the Yangtze River (Changjiang), spanning from the mouth (33 degrees N) similar to 1000 km southward to the southwestern corner of the Taiwan Strait (24 degrees N).
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Structural features off southwestern Taiwan
TL;DR: In this article, the boundary between the Chinese continental margin and the Taiwan orogen can be clearly delineated by the deformation front of the contractional structures, and a complex system of faults, mud diapirs, submarine channels, and sedimentary basins in the offshore area southwest of Taiwan.