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Article Navigation >  Acta Sedimentologica Sinica  > 1997  >  15(1): 152-155

Xie Xiaoan, Wu Qizhi, Lu Huafu. Tectonic Framework and Sedimentary Feature of the Tarim Basin in Paleozoic[J]. Acta Sedimentologica Sinica, 1997, 15(1): 152-155.
Citation: Xie Xiaoan, Wu Qizhi, Lu Huafu. Tectonic Framework and Sedimentary Feature of the Tarim Basin in Paleozoic[J]. Acta Sedimentologica Sinica, 1997, 15(1): 152-155.
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Tectonic Framework and Sedimentary Feature of the Tarim Basin in Paleozoic

  • 1 Department of Earth Sciences Nanjing University 210008;

  • 2 Bureau of Geophysical Prospecting CNPC Hepei Zhuozhou 072751

  • Received Date: 1996-09-25
  • Publish Date: 1997-03-10
  • Between Tianshan and kunlun一Aerjin Mountains lies Tarim Basin, the largest sedimentary basin inchina. The basin has undergone the formation of basement during pre Siian and development sincePhanerozoic and it is agiant complex basin with the histry of a Paleozoic origina lcraton basin overlain bya Mesozoic-Cenozoic foreland basin. The craton basin had been subjected to a rift in nian, a marginalaulacogen in Cambrian-Ordovician and an intracratonic depression basin in Silurian-Permian. The Paleo-wic Erachem is mainly a set of〔arbonate rocks and clastic rocks of marinefacies and the sedimentary anddepressi ng centers experienced several times of shifting during Paleozoic.The Louer Paleowic is thickerin the east than in the west and the Upper Paleozoic is thinner in the east than in the west. All resultedfrom the control of the plate evolution and tectonic framework in Paleozoic.
  • [1] 1 贾承造.姚慧君等.塔里术盆地板块构造演化和主要构造单元地质构造特征.见:童晓光.梁狄刚主编.塔里术盆地油气勘探论文集.乌鲁术齐:新疆科技卫生出版社.1992.

    2 王尚文等.中国石油地质学.北京:石油工业出版社.1983.

    3 顾家裕等.沉积相与油气.北京:石油工业出版社.1994.

    4 贾承造.姚慧君等.塔里术盆地地层系统.见:童晓光.梁狄刚主编.塔里术盆地油气勘探论文集.乌鲁术齐:新疆科技卫生出版社.1992.

    5 谢晓安.工仁德等.塔里术盆地构造特征及其找油方向.石油地震地质1991, 3 ( 2):

    6 杨克明.熊永旭等.中国西北地区板块构造与盆地类型.石油与天然气地质.1992, 13 ( 1):

    7 肖序常.汤耀庆等.新疆北部及其邻区人地构造.北京:地质出版社，1992.

    8潘裕生青藏高原第五缝合带的发现与论证.地球物理学报，1994,37(2)
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  • Received:  1996-09-25
  • Published:  1997-03-10

Tectonic Framework and Sedimentary Feature of the Tarim Basin in Paleozoic

  • 1 Department of Earth Sciences Nanjing University 210008;
  • 2 Bureau of Geophysical Prospecting CNPC Hepei Zhuozhou 072751
  • Received Date: 1996-09-25
  • Publish Date: 1997-03-10

Abstract: Between Tianshan and kunlun一Aerjin Mountains lies Tarim Basin, the largest sedimentary basin inchina. The basin has undergone the formation of basement during pre Siian and development sincePhanerozoic and it is agiant complex basin with the histry of a Paleozoic origina lcraton basin overlain bya Mesozoic-Cenozoic foreland basin. The craton basin had been subjected to a rift in nian, a marginalaulacogen in Cambrian-Ordovician and an intracratonic depression basin in Silurian-Permian. The Paleo-wic Erachem is mainly a set of〔arbonate rocks and clastic rocks of marinefacies and the sedimentary anddepressi ng centers experienced several times of shifting during Paleozoic.The Louer Paleowic is thickerin the east than in the west and the Upper Paleozoic is thinner in the east than in the west. All resultedfrom the control of the plate evolution and tectonic framework in Paleozoic.

Xie Xiaoan, Wu Qizhi, Lu Huafu. Tectonic Framework and Sedimentary Feature of the Tarim Basin in Paleozoic[J]. Acta Sedimentologica Sinica, 1997, 15(1): 152-155.
Citation: Xie Xiaoan, Wu Qizhi, Lu Huafu. Tectonic Framework and Sedimentary Feature of the Tarim Basin in Paleozoic[J]. Acta Sedimentologica Sinica, 1997, 15(1): 152-155.
shu

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