鄂尔多斯盆地奥陶系盐下马家沟组四段云斑灰岩储层的非均质性特征及优质储层的发育环境OA
Heterogeneity of dolomite-spotted limestone reservoirs of the sub-salt fourth member of the Ordovician Majiagou Formation in the Ordos Basin and development environment of high-quality reservoirs
鄂尔多斯盆地奥陶系盐下马家沟组四段是区域勘探热点,其中发育的云斑灰岩是重要的储层类型之一.目前对该储层的非均质性特征、优质储层及控制因素的认识较薄弱,从而制约了全面评价工作的深入及下一步的勘探开发.为此,本文综合运用岩矿学、沉积学、遗迹学和储层地质学等方法,研究储层的非均质性特征,揭示优质储层的类型及发育环境.结果表明,研究区云斑灰岩可划分为发育Glossifungites遗迹相的三维箱状结构和发育Cruziana遗迹相的二维水平迷宫结构两种类型.云斑灰岩发育基质微孔、残余灰泥微孔、白云石晶间孔、白云石晶内微孔、溶蚀孔和裂缝6类储集空间.有效储集空间为潜穴内部的白云石晶间孔,基质内孔隙孤立,由此导致云斑灰岩具有强的非均质性和物性测量的样品尺寸依赖性.全尺寸样品建模分析揭示三维箱状结构云斑灰岩的孔隙度和渗透率分别为3.20%、1.03 mD,二维迷宫结构云斑灰岩的孔隙度和渗透率分别为0.55%、0.18 mD.前者物性优于后者,且在各个方向均具备连通性,是优质储层类型.基于遗迹相和沉积序列等综合分析,表明该优质储层发育的沉积环境为水体能量较高的潮间—浅潮下带.
The sub-salt fourth member of the Ordovician Majiagou Formation in the Ordos Basin is a regional exploration hotspot,and dolomite-spotted limestones form important petroleum reservoirs.Currently,reservoir heterogeneity,high-quality reservoirs and their controlling factors have been poorly understood,limiting in-depth comprehensive evaluation and exploration and development in future.Therefore,with an integrated method of petrography,sedimentology,ichnology and reservoir geology,this paper studies heterogeneity characteristics of the reservoirs and reveal high-quality reservoir types and development environments.The results show that dolomite-spotted limestones in the study area can be classified into two types:three-dimensional box structure with Glossifungites ichnofacies and two-dimensional horizontal maze structure with Cruziana ichnofacies.Six types of reservoir spaces develop in the dolomite-spotted limestone:matrix micro-pores,residual mud micro-pores,dolomite intercrystalline pores,dolomite intracrystalline micro-pores,dissolution pores and fractures.The effective reservoir space is dolomite intercrystalline pores inside burrows and matrix pores are isolated,these lead to strong heterogeneity of dolomite-spotted limestones and sample size dependence of physical property measurement.Modeling analysis of full-size samples reveals that porosity and permeability of the dolomite-spotted limestone with three-dimensional box structure are 3.20%and 1.03 mD,respectively,while those with two-dimensional maze structure are 0.55%and 0.18 mD,respectively.The former has better physical properties and pores are well connected in all directions,making it a high-quality reservoir type.Further comprehensive analyses of ichnofacies and depositional sequences indicate that the depositional environment where this high-quality reservoir develops is the high-energy intertidal to shallow subtidal zone.
袁子彧;王爱国;王前平;罗晓容;魏柳斌;郭玮;曹斌风
中国石油长庆油田公司勘探开发研究院 西安 710018||低渗透油气田勘探开发国家工程实验室 西安 710018西北大学地质学系/大陆演化与早期生命全国重点实验室 西安 710069中国石油长庆油田公司勘探开发研究院 西安 710018||低渗透油气田勘探开发国家工程实验室 西安 710018西北大学地质学系/大陆演化与早期生命全国重点实验室 西安 710069中国石油长庆油田公司勘探开发研究院 西安 710018||低渗透油气田勘探开发国家工程实验室 西安 710018中国石油长庆油田公司勘探开发研究院 西安 710018||低渗透油气田勘探开发国家工程实验室 西安 710018西北大学地质学系/大陆演化与早期生命全国重点实验室 西安 710069
天文与地球科学
鄂尔多斯盆地马家沟组云斑灰岩储层非均质性优质储层
Ordos BasinMajiagou FormationDolomite-spotted limestonesReservoir heterogeneityHigh-quality reservoirs
《地质科学》 2026 (1)
82-99,18
中国石油长庆油田公司重大科技专项"鄂尔多斯盆地深部层系构造—沉积环境、成藏条件与有利勘探区带研究"(编号:2024D1JC06)资助
评论