| 鄂尔多斯地区晚古生代陆相沉积层序地层学研究 |
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| 引用本文： | 侯中健,陈洪德,田景春,刘文均,张锦泉.鄂尔多斯地区晚古生代陆相沉积层序地层学研究[J].矿物岩石,2001,21(3):114-123. |
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| 作者姓名： | 侯中健 陈洪德 田景春 刘文均 张锦泉 |
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| 作者单位： | 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 |
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| 摘 要： | 鄂尔多斯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。
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| 关 键 词： | 层序地层学 陆相沉积 鄂尔多斯地区 二叠系 晚古生代 沉积盆地 |
| 文章编号： | 1001-6872(2001)03-0114-10 |
STUDY ON SEQUENCE STRATIGRAPHY OF CONTINENTAL DEPOSITS IN ORDOS BASIN DURING LATER PALAEOZOIC ERA |
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| 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.STUDY ON SEQUENCE STRATIGRAPHY OF CONTINENTAL DEPOSITS IN ORDOS BASIN DURING LATER PALAEOZOIC ERA[J].Journal of Mineralogy and Petrology,2001,21(3):114-123. |
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| Authors: | 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 |
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| Institution: | 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 |
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| 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. |
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| Keywords: | sequence stratgraphy continental deposit Ordos area Permian Late Palaeozoic |
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