A value of∼ 10− 14 s− 1 is commonly cited as an average geological strain rate. This value
was first suggested for finite strain across an orogen, but based on more limited information …

Since 1990, digital strong-motion accelerographs and global positioning system (GPS)
instruments have been widely deployed in the Taiwan region (Shin et al. 2003; Yu et al …

Abstract The Longitudinal Valley Fault (LVF) in eastern Taiwan is a high slip rate fault (about
5 cm/yr), which exhibits both seismic and aseismic slip. Deformation of anthropogenic …

Offsets of synthetic aperture radar (SAR) images have played an important role in deriving
complete three-dimensional (3-D) surface displacement fields in geoscientific applications …

On 1999 September 21, the Mw 7.6 Chi‐Chi earthquake ruptured a segment of the
Chelungpu Fault, a frontal thrust fault of the Western Foothills of Taiwan. The stress …

Using data at 110 continuous GPS stations from 1 January 2003 to 31 December 2005, we
characterized the surface deformation in Taiwan after the Mw= 7.6 Chi‐Chi earthquake of 21 …

In order to better understand the mode of subduction polarity reversal in the Taiwan–Luzon
arc-continent collision zone, we mapped its crust–mantle boundaries using local earthquake …

Cree** crustal faults often generate a large number of microearthquakes, and less
commonly, they may also produce major earthquakes that rupture the brittle crust. The …

We present 10‐year continuous seismic velocity changes from 2007 to 2017 around the
Longmenshan fault zone, where the 2008 Mw 7.9 Wenchuan earthquake and the 2013 Mw …

Abstract The Longitudinal Valley Fault (LVF, Taiwan) is a fast‐slip** fault (∼ 5 cm/yr),
which exhibits both seismic and aseismic slip. Geodetic and seismological observations …