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Article Navigation >  Acta Sedimentologica Sinica  > 1996  >  14(S1): 206-213

Wu Xiaozhi, Xiang Shuzheng, Zhao Yongde, Wang Xu, Wu Shaozu. The Lithofacies and Paleogeography of Upper Palaeozoic in the Fuhai Area of North Xinjiang[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 206-213.
Citation: Wu Xiaozhi, Xiang Shuzheng, Zhao Yongde, Wang Xu, Wu Shaozu. The Lithofacies and Paleogeography of Upper Palaeozoic in the Fuhai Area of North Xinjiang[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 206-213.
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The Lithofacies and Paleogeography of Upper Palaeozoic in the Fuhai Area of North Xinjiang

  • 1 Research Institute of Exploration and Development, Xinjiang Petroleum Administation Bureau. Karamay 834000;

  • 2 The 05 Engineering Department of Southwest Geology Resource Bureau, Guiyang 610081

  • Received Date: 1995-08-22
  • Publish Date: 1996-12-31
  • The Fuhai area of north Xinjiang is situated in the convergent zone between Siberia Plate and Kazakstan Plate. This area was in an island arc and retroarc basin environment so that its structure activity is violent. There exists many kinds of depositional basins in the Upper Palaeozoic, such as oceanic basin, remnant oceanic basin, island-arc basin, bycontinentalarc basin, intracontinental basin, and so on. There are all kinds of lithofacies: deep-sea,shallow sea, coastal sea, deltaic and fluvial, lacustrine, and swamp facoes. Lots of mixed subfacies zones cause the complex distribution of factes zones. Because of the seawater's withdrawal, continental factes replaced marine factes completely in the Late Carboniferous. Resultantly,the Paleoclimate appeared remarkably different. The Palaeozoic deposition ceased by the end of Early Permian.
  • [1] 1.弗里德曼著，徐怀大译.沉积学原理.科学出版社，1987. 423.

    2.刘宝君等.岩相古地理基础及工作方法.地质出版社，1985. 316.

    3.潭元弼.古生物学简明教程.地质出版社，1983. 270.

    4.肖世禄等.新班北部泥盆系研究.新班科技卫生出版社，1992, 185.

    5.李永妥等.新班北部古地磁研究.新班地质，1992, l0 (4): 228.
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  • Received:  1995-08-22
  • Published:  1996-12-31

The Lithofacies and Paleogeography of Upper Palaeozoic in the Fuhai Area of North Xinjiang

  • 1 Research Institute of Exploration and Development, Xinjiang Petroleum Administation Bureau. Karamay 834000;
  • 2 The 05 Engineering Department of Southwest Geology Resource Bureau, Guiyang 610081
  • Received Date: 1995-08-22
  • Publish Date: 1996-12-31

Abstract: The Fuhai area of north Xinjiang is situated in the convergent zone between Siberia Plate and Kazakstan Plate. This area was in an island arc and retroarc basin environment so that its structure activity is violent. There exists many kinds of depositional basins in the Upper Palaeozoic, such as oceanic basin, remnant oceanic basin, island-arc basin, bycontinentalarc basin, intracontinental basin, and so on. There are all kinds of lithofacies: deep-sea,shallow sea, coastal sea, deltaic and fluvial, lacustrine, and swamp facoes. Lots of mixed subfacies zones cause the complex distribution of factes zones. Because of the seawater's withdrawal, continental factes replaced marine factes completely in the Late Carboniferous. Resultantly,the Paleoclimate appeared remarkably different. The Palaeozoic deposition ceased by the end of Early Permian.

Wu Xiaozhi, Xiang Shuzheng, Zhao Yongde, Wang Xu, Wu Shaozu. The Lithofacies and Paleogeography of Upper Palaeozoic in the Fuhai Area of North Xinjiang[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 206-213.
Citation: Wu Xiaozhi, Xiang Shuzheng, Zhao Yongde, Wang Xu, Wu Shaozu. The Lithofacies and Paleogeography of Upper Palaeozoic in the Fuhai Area of North Xinjiang[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 206-213.
shu

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