鄂尔多斯盆地马五5亚段沉积微相分布及演化
第44卷 第5期
煤田地质与勘探 Vol. 44 No.5 2016年10月 COAL GEOLOGY & EXPLORA TION Oct . 2016
收稿日期: 2015-05-08
基金项目: 国家科技重大专项课题(2011ZX05004-006)；四川省重点学科建设项目(SZD0414)
Foundation item ：National Science and Technology Major Project(2011ZX05004-006)；Key Discipline Construction Projects in Sichuan Province (SZD0414)
作者简介: 包洪平(1967—)，男，甘肃兰州人，硕士，教授级高级工程师，从事油气地质研究. E-mail ：baohp67@https://www.wendangku.net/doc/488232471.html,
通信作者：张云峰(1982—)，男，河南鹿邑人，工学博士，讲师，从事碳酸盐岩沉积学、储层地质学研究. E-mail ：zhyf@https://www.wendangku.net/doc/488232471.html, 引用格式: 包洪平，张云峰，王前平，等. 鄂尔多斯盆地马五5亚段沉积微相分布及演化[J]. 煤田地质与勘探，2016，44(5)：16–21.
BAO Hongping ，ZHANG Yunfeng ，WANG Qianping ，et al. Distribution and evolution of sedimentary microfacies of submember 5 Majiagou Formation in the Ordos basin[J]. Coal Geology & Exploration ，2016，44(5)：16–21. 文章编号: 1001-1986(2016)05-0016-06
鄂尔多斯盆地马五5亚段沉积微相分布及演化
包洪平1，张云峰2，王前平1，董兆雄2，武春英1，杨西燕2
(1. 中石油长庆油田分公司勘探开发研究院，陕西 西安 710018；
2. 西南石油大学地球科学与技术学院，四川 成都 610500)
摘要: 岩性及沉积环境的差异是鄂尔多斯盆地下奥陶统马家沟组马五5亚段储层非均质性的重要因素，根据岩石类型、沉积构造及颜色等特征及其与沉积微相的关系，研究区马五5亚段可分为盆缘坪和台内盆地两个亚相及缘内(膏)云质洼地、缘内云坪、缘内灰坪、缘内云灰–灰云坪、盆地(膏)云质洼地、灰云–云灰质盆地及灰质盆地等微相。沉积微相平面上表现为，马五52时期，鄂尔多斯盆地基底抬升，中央古隆起带露出水面；北部地区发育缘内云坪–云质洼地、缘内灰云–云灰坪和灰质盆地；西部地区为缘内云坪–云质洼地、缘内灰云–云灰坪；中部地区为灰质盆地，间夹云灰盆地及盆内云质洼地；马五51时期，北部地区主要发育缘内云坪–云质洼地；西部地区为缘内云坪–云质洼地；中部地区为灰质盆地及盆内云质洼地。盆缘坪和台内盆地的低洼处有利于发生同生期后回流渗透白云化作用，对生成较大规模的泥粉晶白云岩具有重要的意义。
关 键 词：沉积微相；沉积演化；碳酸盐岩；马五5亚段；鄂尔多斯盆地
中图分类号：TE16 文献标识码：A DOI: 10.3969/j.issn.1001-1986.2016.05.003
Distribution and evolution of sedimentary microfacies of submember 5
Majiagou Formation in the Ordos basin
BAO Hongping 1, ZHANG Y unfeng 2, W ANG Qianping 1, DONG Zhaoxiong 2, WU Chunying 1, Y ANG Xiyan 2
(1. Research Institute of Exploration and Development , Petro China Changqing Oilfield Company , Xi an 710018, China ;
2. School of Geoscience and Technology , Southwest Petroleum University , Chengdu 610500, China)
Abstract: The difference between lithology and depositional environment is the main cause of reservoir heteroge-neity in submember 5 Majiagou Formation of Lower Ordovician in the Ordos basin. According rock types, sedi-mentary structures, color and its relationship with sedimentary environment, two subfacies and seven microfacies in submember 5 Majiagou Formation are classified. subfacies include basin-marginal tidal flat and intra-platform basin. The former can be furtherly divided into four types microfacies, such as intra-platform margin (gypsum) dolomite depression, intra-platform margin dolomite tidal flat, intra-platform margin calcitic tidal flat and in-tra-platform margin dolomite calcitic–calcitic dolomite tidal flat. The latter can be furtherly divided into three types microfacies, such as basin (gypsum) dolomite depression, dolomite calcitic–calcitic dolomite basin and calcitic ba-sin. In the stage of submember 5-1 Majiagou Formation, Ordos basin basement uplift, the ancient land expand, re-duce sea level, shallow sea, the ancient central uplift belt out of the water are the performance of sedimentary mi-crofacies plane. North area is mainly developing intra-platform margin dolomite tidal flat-dolomite depression, in-tra-platform margin dolomite calcitic-calcitic dolomite tidal flat and calcitic basin. West area develop in-tra-platform margin dolomite tidal flat-dolomite depression, intra-platform margin dolomite calcitic-calcitic dolo-mite tidal flat. Center area develop calcitic basin, and mix dolomite calcitic basin and basin dolomite depression. In the stage of submember 5-2 Majiagou Formation, north area mainly developing intra-platform margin dolomite tidal flat and dolomite depression. Secondary microfacies include dolomite calcitic–calcitic dolomite tidal flat, cal-万方数据