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川中地区上三叠统须四段砂体成因组合及对油气富集的影响
引用本文:谢武仁,李熙喆,杨威,张满郎,谢增业,金蕙.川中地区上三叠统须四段砂体成因组合及对油气富集的影响[J].沉积学报,2009,27(6):1084-1092.
作者姓名:谢武仁  李熙喆  杨威  张满郎  谢增业  金蕙
作者单位:中国石油勘探开发研究院廊坊分院河北廊坊065007
基金项目:中国石油天然气股份有限公司科技攻关项目 
摘    要:川中地区上三叠统须四段砂体厚度大,沉积稳定,为近物源区的三角洲沉积特征。沉积过程中,物源供应速率与可容纳空间增长关系的变化,导致须四段砂体自下而上由水退式、河道式和水进式三种不同成因类型的砂组纵向叠合而成;层序界面之上的河道式砂组为物性最好的成因砂体。水退式砂组主要由高能削截式河道、削截式河口坝和远砂坝组成,河道式砂组主要包括冲蚀下切式河道和高能削截式河道,水进式砂组主要包括低能河道、低能削截式河道、完整式河口坝和下缺式河口坝。由于不同的砂体组合,不同成因砂体间形成了不同的成岩相和储集相,河道式砂组以绿泥石衬边和溶蚀成岩相为主,物性好,为好的储集体;水进式砂组由压实和胶结相为主,物性较差;水退式砂组中溶蚀相和胶结相发育,物性较好,为中等的储集体。由于河道式砂组与水退式砂组呈沉积不整合相接触,呈现镶嵌关系,对天然气的运移起到通道作用,同时河道式砂组在平面上分布范围大,其中的高能削截式河道沉积稳定,为油气的富集提供了足够的空间,向上的水进式砂组发生储层致密化,形成有利的盖层,使河道式砂组发育区成为川中天然气富集的有利部位。

关 键 词:川中地区上三叠统须四段砂体成因河道砂体砂体组合
收稿时间:1900-01-01

Genetic Combination of the Sandbody in the Fourth Members of Xujiahe Formation (Upper Triassic) and Its Influence on Oil and Gas Reservoirs
XIE Wur-en,LI Xi-zhe,YANG Wei,ZHANG Man-lang,XIE Zeng-ye,JIN Hui.Genetic Combination of the Sandbody in the Fourth Members of Xujiahe Formation (Upper Triassic) and Its Influence on Oil and Gas Reservoirs[J].Acta Sedimentologica Sinica,2009,27(6):1084-1092.
Authors:XIE Wur-en  LI Xi-zhe  YANG Wei  ZHANG Man-lang  XIE Zeng-ye  JIN Hui
Institution:The Geology Institute of Langfang Branch, Petroleum Exploration and Development Research Institute,Langfang Hebei065007
Abstract:The sandbody of Upper Triassic Xu 4 member in central Sichuan basin is thick,continuous sedimentation,and characterized by shore-shallow lacustrine-delta front-delta plain which is proximal.During sedimentation,there were different accommodation space /sedimentary supply values,the Xu 4 member sandbody consists of three vertical superposed types which is regressive,channel and transgressive from bottom to top;and the channel sandbody composition on sequence boundary is the best genetic sandbody.Regressive s...
Keywords:central Sichuan Basin  Upper Triassic series  Xu 4 member  genesis of sand body  channel sand  combination of sandbody
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