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  4. ODP/IODP海洋鑽探計畫─子計畫七:南海北部板塊邊界表面跡之特徵及分佈
 
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ODP/IODP海洋鑽探計畫─子計畫七:南海北部板塊邊界表面跡之特徵及分佈

Date Issued
2003
Date
2003
Author(s)
俞何興
DOI
912611M002018
URI
http://ntur.lib.ntu.edu.tw//handle/246246/14831
Abstract
Marine seismic reflection profiles offshore SW Taiwan combined onland geological data are used to investigate distribution and nature of the deformation front west of Taiwan. Locations of the fronatal structure west of Taiwan are generally connected into a continuous line, although the alignment of frontal structures is offset by strike-slip faults. The deformation front begins from the northern Manila Trench near 21 N and continues northward along the course of the Penghu Submarine Canyon in a nearly N-S direction north of 21 N until reaches around 22 15 N at the upper reach of the Penghu Canyon. The deformation front then changes its directions sharly to northeast. It connects to the Chungchou anticline or the Tainan anticline in the coastal plain and continues northwards along the outer Western Foothills to the northern coast of Taiwan near 25 N. Characteristics of structural style, strain regime, sedimentation and tectonics vary along the trend of the deformation front. Ramp anticline, diapiric intrusion and incipient thrust fault are commonly associated with the deformation front. Variations of structural style along strike of the deformation can be related to different stages of oblique collision in Taiwan. The collision front west of 2 Taiwan can be considered as a boundary of strain regime separating contraction in the Taiwan orogen and extension west of the collision zone. The deformation front east of the Tainan Basin and its northward extension along the outer limit of the Western Foothills is the surface trace separating the foreland thrust belt from the nearby foredeep, not a boundary between the Chinese and Taiwan margins. The submarine deformation front off SW Taiwan is the surface trace separating the submerged Taiwan orogenic wedge from the Chinese passive continental margin, not a surface trace of plate boundary between the Eurasian and the Philippine Sea plates.
Subjects
Deformation Front
Distribution
Nature
Seismics
Taiwan
SDGs

[SDGs]SDG14

Publisher
臺北市:國立臺灣大學海洋研究所
Type
report
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912611M002018.pdf

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(MD5):5c302c09e72b1fd5d06f221dd3add479

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