Eogenetic karst and its control on reservoirs in the Ordovician Majiagou Formation, eastern Sulige gas field, Ordos Basin, NW China
在奥陶纪 Majiagou 形成的水库上的 Eogenetic 石灰岩地区常见的地形和它的控制,东方 Sulige 煤气的地, Ordos 盆, NW 中国作者机构:State Key Laboratory of Oil and Gas Reservoir Geology and ExploitationSouthwest Petroleum UniversityChengdu 610500China Department of Key Laboratory of Carbonate Reservoir of CNPCSouthwest Petroleum UniversityChengdu 610500China Exploration and Development Research Institute of PetroChina Changqing Oilfield CompanyXi’an 710018China Yihuang Natural Gas Department of PetroChina Changqing Oilfield CompanyXi’an 710018China PetroChina Hangzhou Research Institute of GeologyHangzhou 310023China
出 版 物:《Petroleum Exploration and Development》 (石油勘探与开发(英文版))
年 卷 期:2020年第47卷第6期
页 面:1246-1261页
核心收录:
学科分类:0820[工学-石油与天然气工程] 08[工学] 082002[工学-油气田开发工程]
基 金:Supported by the China National Science and Technology Major Project(2016ZX05004006-001-002) CNPC-Southwest Petroleum University Innovation Consortium Technology Cooperation Project
主 题:porous reservoir reservoir characteristics eogenetic karst dolomite Majiagou Formation Ordovician Sulige gas field Ordos Basin
摘 要:To further ascertain the origin of the Ordovician Majiagou Formation reservoirs in the Ordos Basin,the M54-M51 sub-members of the Ordovician Majiagou Formation in the eastern Sulige gasfield of Ordos Basin were taken as examples to analyze the vertical development characteristics of eogenetic karst and to discover the dissolution mechanism and its control on reservoirs through observation of a large number of cores and thin *** to detailed analysis of petrologic characteristics,the reservoir rock types include micritic dolomite,grain dolomite and microbialite which have mainly moldic pore,intergranular(dissolved)pore,and(dissolved)residual framework pore as main reservoir space *** study area developed upward-shallowing sequences,with an exposure surface at the top of a single upward-shallowing *** karst systems under the exposure surface had typical exposure characteristics of early dissolution and filling,indicating these reservoirs were related to the facies-controlled eogenetic *** the increase of karstification intensity,the reservoirs became worse in physical properties.