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central asian fold region
相关语句
  中亚褶皱区
     ON TECTONIC EVOLUTION OF CENTRAL ASIAN FOLD REGION ACHIEVEMENT REVIEW ON RECENT STUDIES BY RUSSIAN GEOLOGISTS
     中亚褶皱区构造演化问题———俄罗斯学者近年研究成果评价
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  “central asian fold region”译为未确定词的双语例句
     Russian geologists divided the Central Asian fold region into two kinds of tectonic provinces: mosaic and linear.
     俄罗斯地质学者把中亚褶皱区划分为两类构造区:镶嵌构造区和线状构造区。
短句来源
  相似匹配句对
     ON TECTONIC EVOLUTION OF CENTRAL ASIAN FOLD REGION ACHIEVEMENT REVIEW ON RECENT STUDIES BY RUSSIAN GEOLOGISTS
     中亚褶皱区构造演化问题———俄罗斯学者近年研究成果评价
短句来源
     Russian geologists divided the Central Asian fold region into two kinds of tectonic provinces: mosaic and linear.
     俄罗斯地质学者把中亚褶皱区划分为两类构造区:镶嵌构造区和线状构造区。
短句来源
     The Ethnic and Religious Problems in Central Asian Region in the Soviet Period
     苏维埃时期的中亚民族宗教问题
短句来源
     (5) the central Pacific region.
     (Ⅴ)太平洋中部区。
短句来源
     Shanghai, the node in the central region;
     上海将成为我国中部的集装箱枢纽港;
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Russian geologists divided the Central Asian fold region into two kinds of tectonic provinces: mosaic and linear. Recent studies considered that the former′s formation was resulted from the accretion of continental margins, occured in Late Riphean, Middle Late Cambrian, Middle Late Ordovician, and Middle Late Silurian; and the later consists of Variscan and Indosinian fold belts, resulted from the continental collision. The evolution of mosaic and linear tectonic provinces is related to the paleoasian...

Russian geologists divided the Central Asian fold region into two kinds of tectonic provinces: mosaic and linear. Recent studies considered that the former′s formation was resulted from the accretion of continental margins, occured in Late Riphean, Middle Late Cambrian, Middle Late Ordovician, and Middle Late Silurian; and the later consists of Variscan and Indosinian fold belts, resulted from the continental collision. The evolution of mosaic and linear tectonic provinces is related to the paleoasian ocean and the paleotethyan ocean respectively. Some of their conclusions are doubtable, because of less complete understanding of Chinese geological literature. For example, the question of the Inner Mongolian Ocean existed in Late Paleozoic Early Mesozoic and the character and evolution of the paleoasian ocean.

俄罗斯地质学者把中亚褶皱区划分为两类构造区:镶嵌构造区和线状构造区。近年来的研究认为前者是由于陆缘增生作用而形成的,增生作用发生于晚里菲,中—晚寒武世,中—晚奥陶世和中—晚志留世;后者包括华力西和印支褶皱带,是大陆碰撞的产物。镶嵌构造区和线状构造区的演化分别与古亚洲洋和古特提斯洋有关。由于对我国地质文献缺乏较全面的了解,他们的某些结论例如内蒙古洋在晚古生代到早中生代的存在和古亚洲洋的性质及演化等问题都是不妥的,作者将对此进行讨论

 
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