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Please use this identifier to cite or link to this item: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/24955

Title: Formation of the Taiwan Island as a Solitary Wave along the Eurasian Continental Plate Margin: Magnetic and Seismological Evidence
Authors: Chengsung Wang;Chih-Ping Huang;Lei-Yui Ke;Wen-Ju Chien;Su-Kun Hsu;Chun-Tien Shyu;Win-Bin Cheng;Chao-Shing Lee;Louis S. Teng
Contributors: NTOU:Institute of Applied Geosciences
國立臺灣海洋大學:應用地球科學研究所
Keywords: Taiwan island;Oblique lithospheric convergence;Solitary wave;Mountain building and collapsing;Magnetic and seismological evidence
Date: 2002-09
Issue Date: 2011-10-20T08:18:31Z
Publisher: TAO
Abstract: abstract:The Philippine Sea plate moves northwestward, with respect to the Eurasian plate, and produces the Ryukyu subduction system (including the Ryukyu trench, the Ryukyu arc and the Okinawa trough) and the Manila subduction system (including the Manila trench and the Luzon arc) with opposite polarity of subduction on the plate boundary along the Ryukyu-Taiwan-Luzon region. The transition zone between these two subduction systems is the Taiwan island, with vigorous mountain building in the south and southwestward as a solitary wave along the Eurasian continental plate margin, with a speed of about 7cm/y. In this paper, we describe the occurrence environment for this phenomenon, with morphological, magnetic and seismological evidence.
The shifting oblique lithospheric convergence of the Philippine Sea plate with the Eurasian continental plate margin causes the transient solitary wave of the Taiwan island. The convergences has squeezed the tectonic zones near the Taiwan island. The convergence has squeezed the tectonic zones near the plate boundary tightly and uplifted has squeezed the tectonic zones near the plate boundary tightly and uplifted the transition zone that is the Taiwan island. When the convergence site migrates southwestward along the continental plate margin, the squeezed parts of these tectonic zones are released again and spread, by the following tensional stress due to the northward subduction of the Philippine Sea plate. Therefore, the area of Taiwan island does not necessarily increase substantially with geological time. In order to better understand the lithospheric interaction in the Taiwan area, we also proposed a lithospheric convergence model in this paper.
Relation: 13(3), pp.339-354
URI: http://ntour.ntou.edu.tw/handle/987654321/24955
Appears in Collections:[應用地球科學研究所] 期刊論文

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