塔河油田托甫台地区奥陶系一间房组碳酸盐岩储层特征及主控因素

CHARACTERISTICS AND MAJOR CONTROLLING FACTORS OF CARBONATES RESERVOIR IN THE MIDDLE ORDOVICIAN YIJIANFANG FORMATION, TUOFUTAI AREA, TAHE OILFIELD

  • 摘要: 通过对塔河油田托甫台地区30多口钻井录井、测井、试油、地球物理等第一手资料系统分析,结合岩心、薄片观察和地化分析等研究,认为区内奥陶系一间房组储层基质孔隙度较低,溶蚀孔、洞、缝和构造缝是主要的储集空间,储层类型在平面上具有"南北分带、东西分异"的特征。加里东中期是该区岩溶储层形成的关键时期,古地貌、断裂或裂缝作用、高能礁滩体等是控制储层发育的重要因素,表现出明显的层控和断控性。由此预测有利储层位于加里东中期古地貌高部位或岩溶残丘、断裂和裂缝密集带与高能礁滩体的复合部位,主要分布在托甫台中、北部地区。

     

    Abstract: Based on analysis of 30 wells data of logging,well logging,oil production test,geophysical,and rock core and rock thin-section observation,the results show dissolved pores and/or caves,factures are the main reservoir spaces with low matrix porosity in Middle Ordovician Yijianfang Formation,Tuofutai area of Tahe Oilfield.On the plane the reservoir types have the feature of "north-south zoning distribution,east-west heterogeneity".The karst reservoirs mainly formed in middle Caledonian and were controlled by such factors as paleo-geomorphology,faults or fractures,lithology and facies,etc.,showing distinct features of fault-controlled and strata-bound.Thus it is predicted that the areas of favorable reservoir rocks would be developed in the congruent sites of the high position of Caledonian paleo-geomorphology,concentration area of faults or fractures and high energy reef-flat facies,which are mainly distributed in the middle and northern part of Tuofutai area.

     

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