| 中国板块构造的轮廓 |
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| A PRELIMINARY STUDY OF PLATE TECTONICS OF CHINA |
| 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. |
| LI Chun-yu,WANG Quan,ZHANG Zhi-meng,LIU Xue-ya.1980.A PRELIMINARY STUDY OF PLATE TECTONICS OF CHINA[J].Acta Geoscientica Sinica,2(1):11-22. |
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