| 中国板块构造的轮廓 |
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| 引用本文： | 李春昱,王荃,张之孟,刘雪亚.中国板块构造的轮廓[J].地球学报,1980,2(1):11-22. |
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| 作者姓名： | 李春昱 王荃 张之孟 刘雪亚 |
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| 摘 要： | <正> 一、前言 中国大地构造研究已有数十年历史。早在四十年代中期黄汲清发表了“中国主要地质构造单位”,其后又有各种不同学术观点的中国大地构造文献问世。但从板块构造观点研究中国大地构造则开展的很晚,不过为近数年间之事。中国幅员广大,地质构造复杂,以往的地质资料又缺乏有关板块构造的记载,因而现在要论述全国的板块构造,很感资料的不足。这里只能讲一个大致的轮廓,有些地方也还只是一些设想。
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A PRELIMINARY STUDY OF PLATE TECTONICS OF CHINA |
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| LI Chun-yu,WANG Quan,ZHANG Zhi-meng and LIU Xue-ya.A PRELIMINARY STUDY OF PLATE TECTONICS OF CHINA[J].Acta Geoscientia Sinica,1980,2(1):11-22. |
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| Authors: | LI Chun-yu WANG Quan ZHANG Zhi-meng and LIU Xue-ya |
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| Abstract: | From an examination of the tectonic evolution since the beginning ofPhanerozoic, four palaeo--plates can be divided in China and the adjacentregions. China plate lies in the middle, Siberia plate including Siberia Massifand Angara--Mongolia Geosyncline along its southern margin in the north,India plate including India Massif and the south Tethys Ceosyncline in thesouthwest, and Pacific plate in the southeast. The three sutures between these plates are the Junggar--Solon Suture, the Yarlung Zangbo--Indus Suture and the Taiwan Longitudinal Valley Suture respectively(Fig). The nucleus of China plate is the Tarim-Sino-Korean Massif, which stretches through Chinese territory from west to east, and appears to be a platform or shield composed of Archaean and Proterozoic metamorposed basement. |
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