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  4. Strike-slip faults offshore southern Taiwan: implications for the oblique arc-continent collision processes
 
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Strike-slip faults offshore southern Taiwan: implications for the oblique arc-continent collision processes

Resource
Tectonophysics 274 (1-3): 25-39
Journal
Tectonophysics
Journal Volume
274
Journal Issue
1-3.
Pages
25-39
Date Issued
1997
Date
1997
Author(s)
Fuh, Shi-Chie
Liu, Char-Shine  
Lundberg, Neil
Reed, Donald L.
DOI
10.1016/S0040-1951(96)00296-X
URI
http://ntur.lib.ntu.edu.tw//handle/246246/173881
http://ntur.lib.ntu.edu.tw/bitstream/246246/173881/1/08.pdf
Abstract
Taiwan is the site of present-day oblique arc-continent collision between the Luzon arc of the Philippine Sea plate and the Chinese continental margin. The major structural pattern revealed from marine geophysical studies in the area offshore southern Taiwan is that of a doubly-vergent orogenic belt, bounded by significant zones of thrusting on the west and east of the submarine accretionary wedge. Due to the oblique collision process, strike-slip faults could play an important role in this convergent domain. Topographic lineaments revealed from new digital bathymetry data and seismic reflection profiles confirm the existence of three sets of strike-slip faults in the collision-subduction zone offshore southern Taiwan: the N-S-trending left-lateral strike-slip faults within the Luzon volcanic arc, the NE-SW-trending right-lateral strike-slip faults across the accretionary wedge, and the NNE-SSW-trending left-lateral strike-slip faults lie in the frontal portion of the accretionary wedge. These strike-slip faults overprint pre-existing folds and thrusts and may convert into oblique thrusts or thrusts as the forearc blocks accrete to the mountain belt. A bookshelf rotation model is used to explain the observed geometrical relationships of these strike-slip fault systems. Based on this model, the counter-clockwise rotation of the forearc blocks in the area offshore southern Taiwan could have caused extrusion of the accretionary wedge material into the forearc basin. The originally continuous forearc basin is thus deformed into several closed and separate proto-collisional basins such as the Southern Longitudinal Trough and Taitung Trough. A tectonic evolution model which emphasizes on the development of various structures at different stages of the oblique arc-continent collision for the Taiwan mountain belt is proposed.
Subjects
Bookshelf rotation; Oblique collision; Strike-slip faults
SDGs

[SDGs]SDG14

Other Subjects
arc-continent collision; arc/continent collision; faults; lineament; marine geophysics; oblique collision; Philippine Sea plate; plate convergence; strike slip fault; strike-slip fault; Luzon Strait; Philippines, Luzon; Taiwan
Type
journal article
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08.pdf

Size

1.06 MB

Format

Adobe PDF

Checksum

(MD5):4a939496f8208ca18f6eea46a5386362

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