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鄂尔多斯盆地下奥陶统马家沟组障壁潟湖沉积相模式及有利储层分布规律
引用本文:周进高,张帆,郭庆新,邓红婴,辛勇光.鄂尔多斯盆地下奥陶统马家沟组障壁潟湖沉积相模式及有利储层分布规律[J].沉积学报,2011,29(1):64-71.
作者姓名:周进高  张帆  郭庆新  邓红婴  辛勇光
作者单位:中国石油杭州地质研究院杭州310023
基金项目:国家科技重大专项资助(编号:2008ZX05004-002)资助
摘    要:依据鄂尔多斯盆地古构造古地理背景、古水动力以及古气候条件,结合单井沉积相分析建立了马家沟组障壁潟湖沉积相模式,该模式分三个阶段即与海侵期相对应的以灰岩沉积为主的障壁潟湖沉积阶段(阶段Ⅰ)、与海退相对应的以灰岩夹蒸发岩沉积为主的障壁咸化潟湖沉积阶段(阶段Ⅱ)和与低海平面期对应的以膏岩盐沉积为主的障壁膏盐湖沉积阶段(阶段Ⅲ...

关 键 词:鄂尔多斯盆地  马家沟组  障壁潟湖  沉积相模式  储层预测
收稿时间:1900-01-01

Barrier-Lagoon Sedimentary Model and Reservoir Distribution Regularity of Lower-Ordovician Majiagou Formation in Ordos Basin
ZHOU Jin-gao,ZHANG Fan,GUO Qing-xin,DENG Hong-ying,XING Yong-guang.Barrier-Lagoon Sedimentary Model and Reservoir Distribution Regularity of Lower-Ordovician Majiagou Formation in Ordos Basin[J].Acta Sedimentologica Sinica,2011,29(1):64-71.
Authors:ZHOU Jin-gao  ZHANG Fan  GUO Qing-xin  DENG Hong-ying  XING Yong-guang
Institution:Hangzhou Research Institute of Geology, PetroChina, Hangzhou 310023
Abstract:Lower Ordovician Majiagou Formation is composed of six members in which Ma1,Ma3 and Ma5 are evaporate including dolomite,anhydrite and salt and Ma2,Ma4,Ma6 are limestone with dolomite in Ordos Basin.Majiagou Formation is formed by cyclic sedimentation by intermeshed evaporite and carbonate.Upwarps around the basin and a downwarp in the centre of the basin constitute the Early-Ordovician Palaeogeomorphologic pattern.Upwarps as underwater barriers led to exchange limitation between lagoon and exterior sea and...
Keywords:Ordos Basin  Majiagou Formation  barrier lagoon  sedimentary model  reservoir prediction  
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