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湖泊三角洲前缘砂体成因组合形式和分布规律--以鄂尔多斯盆地姬塬白豹地区三叠系延长组为例
引用本文:田景春,陈高武,窦伟坦,夏青松,倪新锋,张翔,聂永生,杨华,付锁堂,付金华,喻健,宋江海.湖泊三角洲前缘砂体成因组合形式和分布规律--以鄂尔多斯盆地姬塬白豹地区三叠系延长组为例[J].成都理工大学学报(自然科学版),2004,31(6):636-640.
作者姓名:田景春  陈高武  窦伟坦  夏青松  倪新锋  张翔  聂永生  杨华  付锁堂  付金华  喻健  宋江海
作者单位:成都理工大学"油气藏地质及开发工程"国家重点实验室,成都,610059;成都理工大学"油气藏地质及开发工程"国家重点实验室,成都,610059;中石油长庆油田分公司;中石油长庆油田分公司;成都理工大学"油气藏地质及开发工程"国家重点实验室,成都,610059;中石油长庆油田分公司
基金项目:四川省重点学科建设项目 , 中国石油天然气总公司资助项目
摘    要:以鄂尔多斯盆地姬塬白豹地区三叠系延长组为例,系统讨论了湖泊三角洲前缘砂体的成因类型及组合形式.从成因类型上看,三角洲前缘砂体包括:(1)水下分流河道砂体;(2)河口坝砂体;(3)远砂坝砂体;(4)席状砂砂体.从组合类型上看主要包括:(1)叠置的水下分流河道砂体;(2)叠置的河口坝砂体;(3)水下分流河道-河口坝组合砂体;(4)席状砂-远砂坝-河口坝组合砂体等.在此基础上,详细论述了三角洲前缘砂体组合形式的时空分布规律.

关 键 词:湖泊三角洲前缘  砂体组合形式  分布规律  鄂尔多斯  三叠系延长组
文章编号:1671-9727(2004)06-0636-05
修稿时间:2004年7月8日

Origin and association types of lake delta front sandstones and their distribution patterns of Triassic Yanchang Formation in Ordos Basin, China
TIAN Jing-chun,CHEN Gao-wu,DOU Wei-tan.Origin and association types of lake delta front sandstones and their distribution patterns of Triassic Yanchang Formation in Ordos Basin, China[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2004,31(6):636-640.
Authors:TIAN Jing-chun  CHEN Gao-wu  DOU Wei-tan
Institution:TIAN Jing-chun~1,CHEN Gao-wu~1,DOU Wei-tan~
Abstract:Taking the Yanchang Formation of Triassic System in Jiyuan and Baibao area in Ordos Basin as example, this paper discusses in detail the origin and association types of lake delta front sandstones and their distribution patterns. The delta front sandstones include (1) subaqueous distributary channel sandstone; (2) channe-mouth bar sandstone; (3) distal bar sandstone and (4) front sheet sandstone. According to association type the sandstones include (1) superimposed distributary channel sandstone; (2) superimposed channel-mouth bar sandstone; (3) subaqueous distributary channel sandstone and channel-mouth bar association sandstone and (4) channel-mouth bar, distal bar and front sheet association sandstones. The distribution of above association types links closely with the vertical evolution and is controlled by provenance supplies, lake level change and basement depression.
Keywords:lake delta front  sandstone association type  distribution pattern  Ordos Basin  Yanchang (Formation) of Triassic System
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