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Ya-Ju Hsu

Researcher at Academia Sinica

Publications -  78
Citations -  3275

Ya-Ju Hsu is an academic researcher from Academia Sinica. The author has contributed to research in topics: Slip (materials science) & Fault (geology). The author has an hindex of 26, co-authored 74 publications receiving 2861 citations. Previous affiliations of Ya-Ju Hsu include California Institute of Technology & National Taiwan University.

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Frictional Afterslip Following the 2005 Nias-Simeulue Earthquake, Sumatra

TL;DR: It is observed that the cumulative number of aftershocks increases linearly with postseismic displacements; this finding suggests that the temporal evolution ofAftershocks is governed by afterslip.

Supporting Online Material for Deformation and Slip Along the Sunda Megathrust in the Great 2005 Nias-Simeulue Earthquake

TL;DR: Measurements from coral microatolls and Global Positioning System stations reveal trench-parallel belts of uplift up to 3 meters high on the outer-arc islands above the rupture and a 1-meter-deep subsidence trough farther from the trench.
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Deformation and Slip Along the Sunda Megathrust in the Great 2005 Nias-Simeulue Earthquake

TL;DR: The Sunda-Andaman megathrust deformation has been studied from coral microatolls and Global Positioning System (GPS) data in this paper, which reveals trench-parallel belts of uplift up to 3 meters high on the outer arc islands above the rupture and a 1-meter-deep subsidence trough farther from the trench.
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Preseismic deformation and coseismic displacements associated With the 1999 Chi-Chi, Taiwan, Earthquake

TL;DR: In this paper, the authors used Global Positioning System (GPS) data acquired during the 1992-1999 period to estimate the coseismic deformation in central Taiwan.
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Fault geometry and slip distribution of the 1999 Chi-Chi, Taiwan earthquake imaged from inversion of GPS data

TL;DR: In this article, a curved fault surface consisting of multiple segments dipping 20-25° best fits the observations of the Chi-Chi, Taiwan earthquake, and the model fault exhibits reverse and left-lateral slip on a 75 km long N-S trending segment.