Tectonic activity inferred from velocity field of GPS measurements in the
Pingtung-Kaohsiung area, southwestern Taiwan
Tai-Yun Liu
Abstract
We use the GPS measurements for investigating the fault surface
activity and crustal deformation patterns in southwestern Taiwan located
the transition zone from collision to subduction. The velocity field in
study area is from 56.3 mm/yr to 19.6 mm/yr along azimuths from 272.4?
to 250? westward. In the western study area, the displacement vectors
show a counterclockwise deviation toward southwestern, which we
explain it in terms of lateral extrusion bounded by the major faults of the
study area. The GPS vectors indicate that the Chishan Fault and the
Deformation Front move with the right-lateral component. In addition,
the Chaochou Fault and the Kaoping Fault are dominated by left-lateral
extrusion.Furthermore, we exploit the GPS data to calculate the strain rate
in study area. The result of strain rate revealed a southward increasing of
extension strain rate and implies that the tectonic extrusion occurs along
the blocks bounded by major faults.
Reference
Ho, W.Y., Hu, J.C., Ching, K.E., Rau, R.J., Chang, T.Y., Hou, C.S., Lin, K.C.,
Tectonic activity inferred from velocity field of GPS measurements in the
Pingtung-Kaohsiung area, southwestern Taiwan
(Abstract)(Full text)
Lacombe, O., Mouthereau, F., Angelier, J., Deffontaines, B., 2001. Structural,
geodetic and seismological evidence for tectonic escape in SW Taiwan.
Tectonophysics 333, 323-345.
(Abstract)(Full text)
胡植慶,2004,高屏地區活動斷層之衛星定位系統測量,2004年台灣活動斷層與地震災害研討會,
76-85頁
(Abstract)(Full text)
Course: Seminar II (for second-year MSc students)