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鄂尔多斯盆地南部镇泾地区延长组的沉积特征

THE SEDIMENTARY CHARACTERISTICS OF YANCHANG FORMATION IN ZHENYUAN AND JINGCHUAN DISTRICTS, SOUTHERN PART OF ORDOS BASIN

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【作者】 张哨楠胡江柰沙文武赵舒高青松

【Author】 ZHANG Shao nan HU Jiang nai (Chengdu University of Technology,Chengdu 610059) SHA Wen wu ZHAO Shu GAO Qing songInstitute of Oil & Natural Gas Exploration and Development, North China Petroleum Bureau,Zhengzhou 450000

【机构】 成都理工学院科技处!成都610059华北石油地质局规划设计研究院!郑州450000

【摘要】 鄂尔多斯南部镇原泾川地区延长组的沉积特征经过多年的资料积累和深入研究 ,发现在延长期沉积物主要来源于盆地西部的隆起 ,沉积相类型主要为正常的河流三角洲和湖泊沉积 ,岩石学特征表明 ,碎屑颗粒均为颗粒支撑 ,没有杂基支撑的结构类型 ,沉积构造组合也表明没有重力流的沉积特征。有利的储集砂体主要为河口砂坝砂体和分流河道砂体。

【Abstract】 The data collection and detailed study of sedimentary environment of Yanchang Formation in Zhengyuan and Jingchuan area revealed that the sediments were originated from the uplift in the western Ordos basin.Normal fluvial delta facies and lacustrine facies were the major sedimentary facies of Yanchang Formation.Lithological character indicated that clastic grains were grain supported and free from matrix support.The sedimentary association showed that there was no sedimentary feature of gravity flow.The favourable reservoir sand bodies were dominated by distributary mouth bar and distributary channel sand bodies.

【基金】 教育部留学回国人员科研启动基金资助项目
  • 【文献出处】 矿物岩石 ,Journal of Mineralogy and Petrology , 编辑部邮箱 ,2000年04期
  • 【分类号】P618.13
  • 【被引频次】142
  • 【下载频次】877
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