R
Ruey Juin Rau
Researcher at National Cheng Kung University
Publications - 79
Citations - 2676
Ruey Juin Rau is an academic researcher from National Cheng Kung University. The author has contributed to research in topics: Fault (geology) & Subduction. The author has an hindex of 28, co-authored 74 publications receiving 2359 citations. Previous affiliations of Ruey Juin Rau include Binghamton University & State University of New York System.
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Taiwan orogeny: thin-skinned or lithospheric collision?
TL;DR: In this paper, the thin-skinned tectonics hypothesis was formulated to explain mainly the geologic and relatively shallow structures in Taiwan orogeny, which can be used continually to test critically hypotheses of the Taiwan Orogeny.
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Tomographic imaging of lithospheric structures under Taiwan
Ruey Juin Rau,Francis T. Wu +1 more
TL;DR: In this paper, the authors obtained tomographic images of the crustal and mantle velocity structures under Taiwan by simultaneous inversion of local earthquake Pwave arrival times for hypocenters and P-wave velocity structures.
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Geometry and structure of northern surface ruptures of the 1999 Mw=7.6 Chi-Chi Taiwan earthquake: influence from inherited fold belt structures
Jian-Cheng Lee,Hao-Tsu Chu,Jacques Angelier,Yu-Chang Chan,Jyr-Ching Hu,Chia-Yu Lu,Ruey Juin Rau +6 more
TL;DR: In this paper, a kinematic model with a 3D fault surface for the 1999 Mw=7.6 Chi-Chi earthquake in central western Taiwan has been characterised by mapping along the northern fault segment.
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Modern vertical deformation rates and mountain building in Taiwan from precise leveling and continuous GPS observations, 2000–2008
TL;DR: In this article, the present-day and geologic vertical displacement field in the active Taiwan orogenic belt was characterized using GPS vertical velocities and precise leveling and 199 continuous GPS measurements from 2000 to 2008.
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Seismic image of the Tarim basin and its collision with Tibet
TL;DR: A broadband seismic deployment in 1998-1999 in southwestern Tarim provided data for imaging the crust and upper mantle across the contact between the Tarim block and the Tibetan Plateau as discussed by the authors.