CAJ | 학술논문

曹妃甸2-1油田沙一段下部发育湖相碳酸盐岩储层，利用岩心观察、铸体薄片、扫描电镜等资料，分析沙一段下部储层岩性、物性及储集空间特征。结果表明，沙一段下部储层岩性主要为生屑云岩，粒间孔、粒间溶孔、生腔体腔孔、粒内溶孔是主要的储集空间类型，储层物性为中孔-中低渗。储层的发育和分布主要受沉积环境和古地貌的控制，沉积微相成果和古地貌恢复结果可以为预测有利相带提供依据。
조비전2-1유전사일단하부발육호상탄산염암저층，이용암심관찰、주체박편、소묘전경등자료，분석사일단하부저층암성、물성급저집공간특정。결과표명，사일단하부저층암성주요위생설운암，립간공、립간용공、생강체강공、립내용공시주요적저집공간류형，저층물성위중공-중저삼。저층적발육화분포주요수침적배경화고지모적공제，침적미상성과화고지모회복결과가이위예측유리상대제공의거。
Carbonate dolostone was widely developed in the bottom of the first member of Shahejie Formation in CFD 2-1 Oilfield.Various data including core description ,casting thin sections and SEM were used to systemically analyze the reservoir lithology ,rock property and reservoir space types .The study indicated that the main reservoir lithology was bio-clastic dolostone;the reservoir spaces were dominated by intergranular pores ,interparticle dissolution pores ,skeletal pores and intragranular dissolved pores;the reservoir had characteristics of medium porosity and low -medium permeability .The reservoir development and distribution were mainly controlled by sedimentary environment and paleogeomorphy , and the comprehensive study results in carbonate sedimentary model and paleogeomorphy restoration can be used to predict the good reservoir distribution effectively .