| 中国满洲里－绥芬河地学断面域古生代构造单元及其地质演化 |
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| 摘 要： | 额尔古纳－兴安地体（ＥＴ）、松嫩－张广才岭地体（ＳＴ）、佳木斯地体（ＳＴ）是断面域古生代具有独立发展演化历史的地质构造单元，ＥＴ与西伯利亚地台具有亲缘性，ＳＴ－ＪＴ与华北和西伯利亚地台均无亲缘关系；ＳＴ与ＪＴ、ＥＴ与ＳＴ－ＪＴ分别沿牡丹江和嫩江断裂拼贴，最终形成统一亚洲大陆的一部分。
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| 关 键 词： | 地体，亲缘，地质演化，构造单元 |
THE CLASSIFICATION OF THE PALEOZOIC TECTONIC UNITS IN THE AREA CROSSED BY M-S GGT |
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| Authors: | Ye Mao Zhang Shihong Wu Fuyuan |
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| Institution: | Department of Earth Sciences |
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| Abstract: | Three terranes have been distingnished in the area crossed by the M-SGGT. The are,from west to east,Erguna-Xing an terrane(ET ),Songnen-Zhangquang cailing terrane(ST)and Jiamusi terrane(JT). Each terrane is characterizedby its unique structure,stratigraphic feattire,geophysical and geochemical data. Itsuggests that there is an affinity of ET with siberia Continent,but the origin of ST andJT is still in paradox. |
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