Assessment of long-term variation in displacement for a GPS site adjacent to a transition zone between collision and subduction |
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Authors: | David Ching-Fang Shih Yih-Min Wu Gwo-Fong Lin Jyr-Ching Hu Yue-Gau Chen Chien-Hsin Chang |
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Institution: | (1) Department of Geosciences, National Taiwan University, Taipei, 10617, Taiwan;(2) Department of Civil Engineering, National Taiwan University, Taipei, 10617, Taiwan;(3) Institute of Nuclear Energy Research, AEC, P.O. Box 3-7, Lungtan, 32546, Taiwan, ROC;(4) Central Weather Bureau, Taipei, 10048, Taiwan |
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Abstract: | A transition and subduction zone adjacent to the Ryukyu Arc, Ryukyu Trench, and Okinawa Trough, extends between southern Japan
and northeastern Taiwan. It is generated during the northwestward subduction of the Philippine Sea Plate, which lies the Eurasian
Plate along the Ryukyu Trench. The movement of the Philippine Sea Plate is hindered at the northeastern corner of Taiwan,
which causes complicated structure of the Philippine Sea Plate at the western end of the Ryukyu subduction zone. Development
of the active subduction and transition boundary near the western Ryukyu Arc is evaluated statistically by using displacements
derived from GPS site data. The statistical model shows that the absolute displacement derived from GPS measurements of nearly
8 years indicates a maximum spatial variation of 0.625 m. Three trends are observed for such long-term progress, and use of
linear regression also reveals quite good consistency between the data and statistic models. Such rate is also elevated following
the trend development. Southeastern and nearly horizontal movement is suggested to the main development of for the site movements,
it is likely related to the tensional activity adjacent to this boundary. |
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Keywords: | GPS Uncertainty Statistics Ryukyu Arc Taiwan |
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