ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
从新疆地学断面的成果讨论中国西北盆-山区的地壳构造演化
  
关键词:the basin-mountain areas in Northwest China  crustal structure  tectonic evolution
基金项目:为“新疆独山子-泉水河地学断面”项目〔原地质矿产部项目(编号 :9501204);国家自然科学基金项目(编号:F49734230);国家新疆305项目编号:(-96-915-07-03),国土资源部科技项目 (编号:20001010201)
作者单位E-mail
刘训 中国地质科学院地质研究所 北京100037 liuxm@cags.net.cn 
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摘要:
A Study of the Crustal Tectonic Evolution in Basin-Mountain Areas of Northwest China in the Light of Xinjiang Geotransect
      Based on the achievements of Geotransect from Dushanzi to Quanshuigou of Xinjiang, this paper deals with the crustal structure and tectonics of such areas of southern Xinjiang as Junggar basin, Tianshan Mountains, Tarim basin and Kunlun Mountains. Some characteristics of the crustal structure and tectonic evolution history of basin-mountain areas in Northwest China are also discussed. The author holds that the tectonic movement of the crust in the basin-mountain areas of Northwest China is mainly attributed to the unhomogeneity of the crust and the upper mantle, including the unhomogeneity of structures and components. It is emphasized in this paper that the present tectonic features of basin-mountain areas are products of Cenozoic crustal activities. Its formation started in Mesozoic or even Late Paleozoic. It is therefore a continuous historical process. Nevertheless, their present frameworks are quite different from those in Mesozoic.
LIU Xun.2005.A Study of the Crustal Tectonic Evolution in Basin-Mountain Areas of Northwest China in the Light of Xinjiang Geotransect[J].Acta Geoscientica Sinica,26(2):105-112.
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