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鄂尔多斯地区晚古生代陆相沉积层序地层学研究

STUDY ON SEQUENCE STRATIGRAPHY OF CONTINENTAL DEPOSITS IN ORDOS BASIN DURING LATER PALAEOZOIC ERA

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【作者】 侯中健陈洪德田景春刘文均张锦泉

【Author】 HOU Zhong jian CHEN Hong de TIAN Jing chun LIU Wen jun ZHANG Jin quan Institute of Sedimentary Geology,Chengdu University of Technology,State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation, Chengdu 610059

【机构】 成都理工学院沉积地质研究所成都理工学院沉积地质研究所 “油气藏地质及开发工程”国家重点实验室四川成都610059“油气藏地质及开发工程”国家重点实验室“油气藏

【摘要】 鄂尔多斯盆地区晚古生代陆相沉积占据了较长的时期 ,基于现代沉积学理论和层序地层学思想 ,本文从鄂尔多斯地区晚古生代沉积盆地的沉积特点出发 ,建立一套比较切合实际的层序地层划分方案 ,研究了该区晚古生代陆相沉积层序地层学 ,比较客观地反映了盆地沉积作用和构造演化历史。

【Abstract】 The Ordos basin experienced a long period of continental deposition during Palaeozoic and therefore,is an ideal place for research of sequence stratigraphy of continental deposits.Through detailed study of stratigraphic correlation and based on the theories of modern sedimentology and sequence stratgraphy,a stratigraphic division was established.In Palaeozoic continental area,the delta deposits ad other lake basin fillings can be classified into 21 sequences which can be subdivided into 5 ultrasequences,and these squences respond well to the evolution of Ordos basin from Shanxi stage of early Permian to Shiqianfeng stage of late Permian.

  • 【文献出处】 矿物岩石 ,Journal of Mineralogy and Petrology , 编辑部邮箱 ,2001年03期
  • 【分类号】P618.13;P539.2
  • 【被引频次】46
  • 【下载频次】461
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