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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2007-03
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Sandstone characteristic and provenance analysis of the Permian Shanxi Formation-Shangshihezi Formation in the northeast of Ordos Basin,China

CHEN An-qing1,CHEN Hong-de1,XIANG Fang1, LIU Wen-jun1,HOU Zhong-jian1,SHANG Yun-zhi2,YE Liming1,LI Jie11.State Key Laboratory of Oil & Gas Reservior Geology and Exploitation,Chengdu University of Technology, Chengdu 610059,China;2.Exploration and Development Research Institute of Daqing Oilfield Company Ltd.,Daqing 163712,China  
This paper analyzes the clastic composition,debris,cathodoluminescence,heavy minerals and paleocurrent of the sandstone of the Permian Shanxi Formation-Shangshihezi Formation in the northeast of Ordos Basin.These evidences display that the provenance derives from the north Yinshan paleoland,the primary cover composed of the Mesoproterozoic sedimentary rock and metamorphic rocks,and the crystallization basement composed of the Paleoproterozoic and Archean metamorphic rocks.By Dickinson triplot of clastic component,most of sands fall in the recycled orogen,and some in mixed and volcanic provenance.All the studies reveal the extension-compression cycle process of the sutural movement between the Siberian plate and North China plate.Consequently,the provenance supply represents obvious cycles.In the process,every early period of the super-long-term cycle formed by regional tectonism is combined with a period of activity regional tectonism and abundant provenance supply.In a word,the types and structural characteristic of basin filling is the response of coupling between the tectonism in provenance area and basin evolution.
【CateGory Index】: P588.21
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