Full-Text Search:
Home|Journal Papers|About CNKI|User Service|FAQ|Contact Us|中文
《Geotectonica Et Metallogenia》 2001-04
Add to Favorite Get Latest Update

ISLANDS-OCEAN STRUCTURAL EVOLUTION OF MID-WESTERN CONTINENT IN INNER MONGULIA

GAO Ji-yuan, WANG Yi-xian, QIOU Yu-zhuo, ZHANG Qian (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China)  
The continent in mid-westhern Inner Mongolia is composed of a microcontinent, three volcanic island arcs and three back-arc basins, which are North China microcontinent, Baiyun Obo back-arc basin, Bainaimiao volcanic island arc, Wendurmiao back-arc basin, Sunitezue-Xilinhaote volcanic island arc, Hegenshan back-arc basin and Erlianhaote-Xilinguole volcanic island arc respectively. At last they have being formed the tectonic framework, after breakup of the volcanic island arcs, subduction, decline and fall of the back-arc basins and arc-microcontinent and arc-arc collision had finished.
【Fund】: 国家科委攀登计划预选项目(95-预-25)资助
【CateGory Index】: P542
Download(CAJ format) Download(PDF format)
CAJViewer7.0 supports all the CNKI file formats; AdobeReader only supports the PDF format.
©2006 Tsinghua Tongfang Knowledge Network Technology Co., Ltd.(Beijing)(TTKN) All rights reserved