靖边气田碳酸盐岩储层沉积-成岩演化模式  

Sedimentary and Diagenetic Evolution Pattern of Reservoir Bed of Carbonate Rock in Jingbian Gasfield of Ordos Basin

作　　者：代金友[1] 铁文斌[2] 蒋盘良[1] 

机构地区：[1]中国石油大学(北京)石油工程学院,北京102249 [2]中国石油新疆油田公司开发公司,新疆克拉玛依834000

出　　处：《科技导报》2010年第11期68-73,共6页Science & Technology Review

基　　金：中国石油天然气股份有限公司重大科技攻关项目(2004110024000244);中国石油天然气集团公司应用基础研究计划项目(06A100103);石油科技中青年创新基金项目(06E1040)

摘　　要：靖边气田主产层次生溶蚀孔洞缝成层连片发育,孔洞缝分布受沉积相和成岩作用双重控制。本文结合98口井岩心观察、1000余块薄片鉴定及多种化验测试资料对储层沉积相、成岩作用进行了系统研究,探讨了储层沉积-成岩演化模式及其对孔洞缝储层发育的控制作用。结果表明,靖边气田储层为蒸发潮坪沉积,并可细分为潮上带泥云坪、膏岩洼地、含膏云坪;潮间带含藻云坪、泥云坪、颗粒滩、潮下带灰坪7种沉积微相;储层埋藏主要经历了白云化、溶解、充填、破裂、交代、压实-压溶、角砾化和重结晶8种成岩作用;储层沉积-成岩演化总体分为沉积同生期、近地表浅埋藏期、抬升风化期和后埋藏期4个阶段;马五11～马五31、马五41a高孔渗段的形成主要受沉积同生期和抬升风化期溶解作用及含膏云坪、含藻云坪和颗粒滩微相控制,而马五32～马五33、马五41b～马五43b、马五5低孔渗段的形成主要受泥云坪、膏岩洼地和灰坪微相控制。Evaporation tidal flat facies are developed in the mid gas field of Ordos Basin.They can be subdivided into 7 microfacies,including mud-dolostone flat of the supralittoral zone,gypseous depression of the supralittoral zone,gypseous dolostone flat of the supralittoral zone,algae-dolostone flat of the intertidal zone,mud-dolostone flat of the intertidal zone,grain bank of the intertidal zone and limestone flat of the subtidal zone.Core observation and thin section analysis indicate that the diagenesis of reservoirs in the syngenesis diagenetic environment,freshwater diagenetic environment and buried diagenetic environment include dolomitization,dissolution,filling cohesion,fracture,replacement,compaction-pressure solution,recrystallization,breccia,etc.Based on the analyses of sedimentary facies and the effect of diagenesis on porosity and permeability characteristics of reservoirs,the sedimentary-diagenetic evolutions of carbonate reservoirs are divided into 4 periods,namely sediment-syngenesis diagenesis period,embedding diagenesis period,near floor,uplift weathering period and late embedding diagenesis period.This unique evolution pattern constitutes vertical 5-layer reservoir architecture,including 2 high porous layers and 3 low porous layers,alternatively distributed.M511～M531 and M541a high porous layers are under the control of the paleokarst in sediment-syngenesis diagenesis period,uplift-weathering period and the microfacies of gypseous dolostone flat,M523～M533,M514b～M534b and M55 low porous layers are under the control of mud-dolostone flat,gypseous depression and limestone flat.

关 键 词：沉积-成岩演化模式 成岩作用 沉积微相 碳酸盐岩 靖边气田 鄂尔多斯盆地 

分 类 号：P618.13[天文地球—矿床学]