National Taiwan Ocean University Institutional Repository:Item 987654321/24955
English  |  正體中文  |  简体中文  |  全文笔数/总笔数 : 28611/40652
造访人次 : 777021      在线人数 : 45
RC Version 4.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜寻范围 进阶搜寻


题名: Formation of the Taiwan Island as a Solitary Wave along the Eurasian Continental Plate Margin: Magnetic and Seismological Evidence
作者: 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
贡献者: NTOU:Institute of Applied Geosciences
关键词: Taiwan island;Oblique lithospheric convergence;Solitary wave;Mountain building and collapsing;Magnetic and seismological evidence
日期: 2002-09
上传时间: 2011-10-20T08:18:31Z
出版者: TAO
摘要: 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.
關聯: 13(3), pp.339-354
显示于类别:[應用地球科學研究所] 期刊論文


档案 描述 大小格式浏览次数



著作權政策宣告: 本網站之內容為國立臺灣海洋大學所收錄之機構典藏,無償提供學術研究與公眾教育等公益性使用,請合理使用本網站之內容,以尊重著作權人之權益。
網站維護: 海大圖資處 圖書系統組
DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 回馈