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Cheng Shoutian, Huang Yanqiu, Fu Xuehong. Paleogeography Reconstruction of the Early- Middle Jurassic Large Ordos Basin and Development and Evolution of Continental Downwarping[J]. Acta Sedimentologica Sinica, 1997, 15(4): 43-49.
Citation: Cheng Shoutian, Huang Yanqiu, Fu Xuehong. Paleogeography Reconstruction of the Early- Middle Jurassic Large Ordos Basin and Development and Evolution of Continental Downwarping[J]. Acta Sedimentologica Sinica, 1997, 15(4): 43-49.

Paleogeography Reconstruction of the Early- Middle Jurassic Large Ordos Basin and Development and Evolution of Continental Downwarping

  • Received Date: 1996-05-12
  • Publish Date: 1997-12-10
  • Based on the genetic relation between sedimentary architecture, paleo- drainage systems and faciesdistribution, and the comparative sedimentology analysis, the paper discussed the uniformity existing inthe primary sediment fillings in the Lower- Middle Jurassic developed of the present Ordos basin and inNingwu and Datong to the east of the basin.The uniformity confirmed that the strata were deposited inthe same Large Ordos basin.The Early- Middle Jurassic paleogeography reconstruction,in terms of fourdeposition stages, revealed the tectonic stages of downwarping- uplifting- redow nwarping and the mi-gration of dynamic setting during the formation and evolution of the basin.The study on the tectonic set-ting for continental downwarping could determine the transformation of Indosinian- Yanshanian tecton-ics and the time of tectonic transformation in North China on a smaller scale.
  • [1] (1) 叶连俊.论华北地台沉积建造,“岩石学研究”.第Ⅰ 辑,北京: 地质出版社, 1982, 1~10.

    (2) 孙国凡,刘景平,柳克琪等.华北中生代大型沉积盆地的发育及其地球动力学背景.石油天然气地质, 1985, 6(3): 278~287.

    (3) 张抗.鄂尔多斯断块构造和资源.西安: 陕西省科学技术出版社, 1989, 193~250.

    (4) 李思田,程守田,杨士恭等.鄂尔多斯盆地东北部层序地层及沉积体系分析.北京: 地质出版社, 1992, 1~12.

    (5) 山西矿业学院,大同矿务局.大同侏罗纪含煤地层沉积环境与聚煤特征.北京: 科学出版社, 1991, 219~230.

    (6) 曹代勇,苏顺金.义马煤盆地的演化及赋存特征.煤田地质与勘探.1988, (6): 11~17.

    (7) 康明.河南义马中生代含煤地层.地层学杂志, 1988, (12): 81 ~93.

    (8) 解习农,程守田,陆永潮.陆相盆地幕式构造旋回与层序构成.地球科学, 1996, 21(1): 27~33.

    (9)Cheng Shoutian, Huang yangiu.Reconstruction of Early - Mid-dle Jurassie Ordos Basin and Its Tectonic Setting, 30 th IGC,Abstracts, 1996, 3(2):: 170
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  • Received:  1996-05-12
  • Published:  1997-12-10

Paleogeography Reconstruction of the Early- Middle Jurassic Large Ordos Basin and Development and Evolution of Continental Downwarping

Abstract: Based on the genetic relation between sedimentary architecture, paleo- drainage systems and faciesdistribution, and the comparative sedimentology analysis, the paper discussed the uniformity existing inthe primary sediment fillings in the Lower- Middle Jurassic developed of the present Ordos basin and inNingwu and Datong to the east of the basin.The uniformity confirmed that the strata were deposited inthe same Large Ordos basin.The Early- Middle Jurassic paleogeography reconstruction,in terms of fourdeposition stages, revealed the tectonic stages of downwarping- uplifting- redow nwarping and the mi-gration of dynamic setting during the formation and evolution of the basin.The study on the tectonic set-ting for continental downwarping could determine the transformation of Indosinian- Yanshanian tecton-ics and the time of tectonic transformation in North China on a smaller scale.

Cheng Shoutian, Huang Yanqiu, Fu Xuehong. Paleogeography Reconstruction of the Early- Middle Jurassic Large Ordos Basin and Development and Evolution of Continental Downwarping[J]. Acta Sedimentologica Sinica, 1997, 15(4): 43-49.
Citation: Cheng Shoutian, Huang Yanqiu, Fu Xuehong. Paleogeography Reconstruction of the Early- Middle Jurassic Large Ordos Basin and Development and Evolution of Continental Downwarping[J]. Acta Sedimentologica Sinica, 1997, 15(4): 43-49.
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