Contemporary deformation of tectonic escape in SW Taiwan from GPS observations, 1995-2005

Kuo-En Ching, Ruey-Juin Rau, Jian Cheng Lee, Jyr Ching Hu

Research output: Contribution to journalArticle

35 Citations (Scopus)

Abstract

The GPS velocity field in SW Taiwan inferred by 103 stations from 1995 to 2005 provides an opportunity to better recognize the contemporary crustal deformation under escaping tectonics. Horizontal velocities relative to the Chinese continental margin from east to west rotate counterclockwise from 42.0 mm/yr to 13.0 mm/yr along azimuths from 246° to 265° across SW Taiwan. The vertical velocity field in SW Taiwan shows a subsidence rate of 5 to 20 mm/yr concentrated on the coastal area of the Pingtung plain and an uplift rate of 10 to 20 mm/yr distributed along the mountain belt. Spatial velocity variation indicates the NE-SW-striking Chishan fault (CHNF) acting as reverse faulting with dextral motion, the N-S-trending Chaochou fault as nearly pure reverse faulting, and the Fengshan transfer fault zone (FTFZ) as left-lateral shearing, intersecting the aforementioned faults. The dominant WNW-ESE shortening and NE-SW dextral shear strain are subject to the fold-and-thrust belt of the Western Foothills west of the CHNF. A NE-SW extension and NW-SE contraction are represented near the FTFZ along the SW coastal area, showing a NW-SE sinistral shear strain. Our GPS data show that the movement of FTFZ greatly enhances the velocities of SW Taiwan rotating from nearly westward direction to WSW direction, sub-parallel to the edge of the basement high (i.e., the rigid indenter) of the Chinese continental margin. The Chishan fault as a boundary fault separates the SW Taiwan into a western deforming domain and an eastern quasi-rigid block. A nearly E-W contraction and N-S extension escaping stress regime is accommodated by N-S-trending ductile flow within the upper mantle and by brittle conjugated-type fracture, formed by the CHNF and the FTFZ, within the crust. The different directions between N-S-trending upper mantle flow and southwestward crustal escape indicate that the crust and upper mantle are decoupled in the tectonic escape process of SW Taiwan.

Original languageEnglish
Pages (from-to)601-619
Number of pages19
JournalEarth and Planetary Science Letters
Volume262
Issue number3-4
DOIs
Publication statusPublished - 2007 Oct 30

Fingerprint

Taiwan
Tectonics
escape
Global positioning system
tectonics
GPS
transfer zone
Faulting
fault zone
Shear strain
Earth mantle
shear strain
upper mantle
continental shelves
contraction
crusts
velocity distribution
continental margin
faulting
Subsidence

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

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title = "Contemporary deformation of tectonic escape in SW Taiwan from GPS observations, 1995-2005",
abstract = "The GPS velocity field in SW Taiwan inferred by 103 stations from 1995 to 2005 provides an opportunity to better recognize the contemporary crustal deformation under escaping tectonics. Horizontal velocities relative to the Chinese continental margin from east to west rotate counterclockwise from 42.0 mm/yr to 13.0 mm/yr along azimuths from 246° to 265° across SW Taiwan. The vertical velocity field in SW Taiwan shows a subsidence rate of 5 to 20 mm/yr concentrated on the coastal area of the Pingtung plain and an uplift rate of 10 to 20 mm/yr distributed along the mountain belt. Spatial velocity variation indicates the NE-SW-striking Chishan fault (CHNF) acting as reverse faulting with dextral motion, the N-S-trending Chaochou fault as nearly pure reverse faulting, and the Fengshan transfer fault zone (FTFZ) as left-lateral shearing, intersecting the aforementioned faults. The dominant WNW-ESE shortening and NE-SW dextral shear strain are subject to the fold-and-thrust belt of the Western Foothills west of the CHNF. A NE-SW extension and NW-SE contraction are represented near the FTFZ along the SW coastal area, showing a NW-SE sinistral shear strain. Our GPS data show that the movement of FTFZ greatly enhances the velocities of SW Taiwan rotating from nearly westward direction to WSW direction, sub-parallel to the edge of the basement high (i.e., the rigid indenter) of the Chinese continental margin. The Chishan fault as a boundary fault separates the SW Taiwan into a western deforming domain and an eastern quasi-rigid block. A nearly E-W contraction and N-S extension escaping stress regime is accommodated by N-S-trending ductile flow within the upper mantle and by brittle conjugated-type fracture, formed by the CHNF and the FTFZ, within the crust. The different directions between N-S-trending upper mantle flow and southwestward crustal escape indicate that the crust and upper mantle are decoupled in the tectonic escape process of SW Taiwan.",
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Contemporary deformation of tectonic escape in SW Taiwan from GPS observations, 1995-2005. / Ching, Kuo-En; Rau, Ruey-Juin; Lee, Jian Cheng; Hu, Jyr Ching.

In: Earth and Planetary Science Letters, Vol. 262, No. 3-4, 30.10.2007, p. 601-619.

Research output: Contribution to journalArticle

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N2 - The GPS velocity field in SW Taiwan inferred by 103 stations from 1995 to 2005 provides an opportunity to better recognize the contemporary crustal deformation under escaping tectonics. Horizontal velocities relative to the Chinese continental margin from east to west rotate counterclockwise from 42.0 mm/yr to 13.0 mm/yr along azimuths from 246° to 265° across SW Taiwan. The vertical velocity field in SW Taiwan shows a subsidence rate of 5 to 20 mm/yr concentrated on the coastal area of the Pingtung plain and an uplift rate of 10 to 20 mm/yr distributed along the mountain belt. Spatial velocity variation indicates the NE-SW-striking Chishan fault (CHNF) acting as reverse faulting with dextral motion, the N-S-trending Chaochou fault as nearly pure reverse faulting, and the Fengshan transfer fault zone (FTFZ) as left-lateral shearing, intersecting the aforementioned faults. The dominant WNW-ESE shortening and NE-SW dextral shear strain are subject to the fold-and-thrust belt of the Western Foothills west of the CHNF. A NE-SW extension and NW-SE contraction are represented near the FTFZ along the SW coastal area, showing a NW-SE sinistral shear strain. Our GPS data show that the movement of FTFZ greatly enhances the velocities of SW Taiwan rotating from nearly westward direction to WSW direction, sub-parallel to the edge of the basement high (i.e., the rigid indenter) of the Chinese continental margin. The Chishan fault as a boundary fault separates the SW Taiwan into a western deforming domain and an eastern quasi-rigid block. A nearly E-W contraction and N-S extension escaping stress regime is accommodated by N-S-trending ductile flow within the upper mantle and by brittle conjugated-type fracture, formed by the CHNF and the FTFZ, within the crust. The different directions between N-S-trending upper mantle flow and southwestward crustal escape indicate that the crust and upper mantle are decoupled in the tectonic escape process of SW Taiwan.

AB - The GPS velocity field in SW Taiwan inferred by 103 stations from 1995 to 2005 provides an opportunity to better recognize the contemporary crustal deformation under escaping tectonics. Horizontal velocities relative to the Chinese continental margin from east to west rotate counterclockwise from 42.0 mm/yr to 13.0 mm/yr along azimuths from 246° to 265° across SW Taiwan. The vertical velocity field in SW Taiwan shows a subsidence rate of 5 to 20 mm/yr concentrated on the coastal area of the Pingtung plain and an uplift rate of 10 to 20 mm/yr distributed along the mountain belt. Spatial velocity variation indicates the NE-SW-striking Chishan fault (CHNF) acting as reverse faulting with dextral motion, the N-S-trending Chaochou fault as nearly pure reverse faulting, and the Fengshan transfer fault zone (FTFZ) as left-lateral shearing, intersecting the aforementioned faults. The dominant WNW-ESE shortening and NE-SW dextral shear strain are subject to the fold-and-thrust belt of the Western Foothills west of the CHNF. A NE-SW extension and NW-SE contraction are represented near the FTFZ along the SW coastal area, showing a NW-SE sinistral shear strain. Our GPS data show that the movement of FTFZ greatly enhances the velocities of SW Taiwan rotating from nearly westward direction to WSW direction, sub-parallel to the edge of the basement high (i.e., the rigid indenter) of the Chinese continental margin. The Chishan fault as a boundary fault separates the SW Taiwan into a western deforming domain and an eastern quasi-rigid block. A nearly E-W contraction and N-S extension escaping stress regime is accommodated by N-S-trending ductile flow within the upper mantle and by brittle conjugated-type fracture, formed by the CHNF and the FTFZ, within the crust. The different directions between N-S-trending upper mantle flow and southwestward crustal escape indicate that the crust and upper mantle are decoupled in the tectonic escape process of SW Taiwan.

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