鄂尔多斯盆地M34区块侏罗系延10段砂质辫状河储层特征及控制因素OA北大核心CSTPCD
Reservoir characteristics and controlling factors of Jurassic Yan 10 Member sandy braided river of M34 Block,Ordos Basin
综合利用岩心、薄片、扫描电镜和储层物性等资料,分析鄂尔多斯盆地M34区块延10段砂质辫状河储层宏微观特征、成岩演化及控制因素,预测有利储层.结果表明:研究区延10段岩石类型丰富,以长石质石英砂岩和岩屑质石英砂岩为主,结构成熟度和成分成熟度较高;储集空间主要为粒间孔、溶蚀孔、晶间孔和微裂缝,发育中孔中喉型、小孔细喉型、细孔微细喉型3类孔隙结构,整体属于低孔低渗型储层,孔渗相关关系较好;发育压实、胶结、溶蚀及交代4类成岩作用,处于中成岩A2期,多阶段的成岩演化使孔隙度降至11.20%~16.30%.优质储层受岩性、沉积、成岩及构造作用共同控制,岩性是优质储层形成的基础,富含石英、长石的细砂岩储层物性最好;沉积为优质储层的形成提供物质条件,心滩和主河道微相储集条件优越,压实和胶结作用是储层减孔的重要原因,其中压实作用是主要因素,溶蚀作用有利于次生孔隙的形成,改善储层物性;构造裂缝是有利储集空间的重要补充,可提高储集性能.延10段储层可划分3类,其中Ⅰ类储层中M30-6X、M34-2、M30-4等井区是有利的勘探目标.该结果对研究区下一步勘探部署具有参考意义.
In order to clarify the characteristics and controlling factors of sandy braided fluvial reservoir of Yan 10 Member in M34 Block,Ordos Basin.The data of core,thin section,scanning electron mi-croscopy and reservoir physical properties were used to discuss the macro and micro reservoir character-istics,diagenesis evolution and controlling factors,as well as predict the favorable reservoir distribu-tion.The results show that the reservoir rock types of Yan 10 Member are abundant,mainly include feldspathic quartz sandstone and lithic quartz sandstone,and the sandstones have good textural maturity and component maturity,the reservoir space is mainly composed of intergranular pores,dissolution pores intercrystal pores and microscope.The pore structure can be divided into three types:mid-pore and mid-throat,small pore and fine throat,fine pore and micro-fine throat.The reservoir physical prop-erties are poor,characterized by low porosity and low permeability as a whole,as well as a relative good correlation between porosity and permeability.The diagenesis mainly includes compaction,cementa-tion,dissolution and metasomatism,the Yan 10 Member is currently in the stage A2 of mesodiagenesis,the porosity decreased to 11.20%-16.30%after multi-stage diagenesis evolution.The high quality reser-voir is controlled by lithologic,sedimentation,diagenesis and tectonism,lithologic is the fundamental conditions for the formation of the high-quality reservoir.The fine sandstones rich in quartz and feldspar have the best physical properties.The sedimentation is the material basis of high-quality reservoir,the physical properties of the main channel and mid-channel bar sandbodies are the best.The compaction and cementation have destructive effects on reservoir physical property,and the compaction is the main factor in making the properties of reservoirs poor.The dissolution can help the forming of secondary pores,improve the physical property of reservoir.Structure fractures are important supplement to form favorable reservoir spaces,which can further improve the physical properties of the reservoir.The fa-vorable reservoir can be divided into three types:Ⅰ,Ⅱ and Ⅲ,the type Ⅰ could be act as the favorable reservoir zones for the future exploration,such as M30-6X,M34-2,M30-4 areas.The results are signif-icant for the next exploration deployment of the research area.
王翔;高吉宏;庞玉东;吴海红;余强;张怀彪;贺昊文
中国石油长庆油田分公司 开发事业部,陕西西安 710018任丘市智科石油技术有限公司,河北任丘 062552中国石油长庆油田分公司第二采油厂,甘肃庆城 745100
石油、天然气工程
储层特征成岩作用控制因素砂质辫状河延10段侏罗系M34区块鄂尔多斯盆地
reservoir characteristicsdiagenesiscontrolling factorssandy braided riverYan 10 Mem-berJurassicM34 BlockOrdos Basin
《东北石油大学学报》 2024 (003)
23-39 / 17
中国石油天然气集团公司重大科技专项(2016E-0505)
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