鄂尔多斯盆地靖边潜台及其周边地区中奥陶统马家沟组马五1-4亚段储层非均质性主要控制因素

作    者:乔琳1, 沈昭国1, 方少仙1, 侯方浩1,傅锁堂2 , 徐黎明2, 马振芳2, 阎荣辉2
单    位:1 西南石油大学;2 中国石油天然气股份有限公司长庆油田分公司
基金项目:四川重点学科建设项目(编号:SZD0414)
摘    要:
鄂尔多斯盆地靖边潜台及相邻区域在马五1-4时总体上为(内)陆棚盆缘坪亚 环境。储层主要岩性为粉晶白云岩及含硬石膏结核和/ 或柱状晶的粉晶白云岩。地层 在岩性上的分布差异是控制储层非均质发育的基础性因素,以含硬石膏结核和/或柱 状晶的粉晶白云岩对研究区更具控制意义。其他主要控制因素还有地质背景、古岩溶 成岩作用、构造裂隙及断层分布等,古地貌、储层有效厚度以及非储层发育程度等对 储层非均质性也具一定影响。靖边潜台为目前天然气主产区,靠近研究区的西侧和东 侧的储集性均较差,西侧地层剥蚀严重,东侧溶蚀作用过于强烈,储集性能均遭到严重 破坏。
关键词:马家沟组;碳酸盐岩储层;储层物性;控制因素;古岩溶;成岩作用;靖边潜台; 鄂尔多斯盆地

The Main Controlled Factors of Heterogeneity of Middle Ordovician Majiagou 5 1-4 Reservoir in Jingbian Buried Platform and Its Periphery Area,Ordos Basin

Author's Name: Qiao Lin, Shen Zhaoguo, Fang Shaoxian, Hou Fanghao,Fu Suotang, Xu Liming, Ma Zhenfang, Yan Ronghui
Institution: Southwest Petroleum University
Abstract:
in the buried Jingbian Buried Platform and its periphery area of Ordos Basin, the sedimentary environment of Middle Ordovician Majiagou 51-4 Sub-member reservoir is generally the inner shelf basin-marginal flat facies. The Majiagou 51-4 reservoir consists of silt-sized crystalline dolostone. Difference of lithology is the basic factor that controls heterogeneity of the reservoir. Silt-sized crystalline dolostone with anhydrite-nodules and/or columnar crystallines plays a predominant role in controlling heterogeneity in this area. Other controlling factors are geologic background, palaeokarst diagenesis, tectonic fissures, fault distribution,etc. In addition, palaeogeo-morphology, effective thickness of reservoir and development of non-reservior are also effective. The main gasproducing zone is in Jingbian Platform but the reservoir did not well-developed or along the west part of the plat-form where strata are severely eroded and the east part rock is heavily dissolved.
Keywords: Middle Ordovician; Majiagou Formation; Carbonate reservoir; Reservoir property; Controlled factors;Palaeokarst; Diagenesis; Jingbian Platform; Ordos basin
投稿时间: 2006-08-07  
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