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Four years of GPS measurements were done since 1996 in southwestern Taiwan in order to investigate crustal deformation and land subsidence. The network of 48 stations revealed the velocity field in the Pingtung Plain. Horizontal velocities range from 31 to 54 mm yr −1 towards azimuths 247° to 273°. They show clear anti-clockwise deviation in the coastal area, consistent with tectonic transtension...
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