首页|鄂尔多斯盆地靖边气田南部马五4亚段沉积相特征及演化

鄂尔多斯盆地靖边气田南部马五4亚段沉积相特征及演化

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奥陶系马家沟组五段4亚段(以下简称"马五4亚段")是靖边气田继马五5亚段之后重要的天然气接替产层之一,但其沉积微相研究相对薄弱,限制了对该气田马五4亚段的碳酸盐岩储层发育及天然气分布有利区的合理、准确预测.以靖边气田南部为例,在已有区域沉积背景研究成果的基础上,通过岩心观察、薄片鉴定和沉积相测井解释,识别研究区马五4亚段的沉积微相类型并刻画其平面展布特征,明确区内马五4亚段各小层沉积微相纵向演化规律.结果表明,靖边气田南部马五4亚段中、西部整体为局限台地亚相沉积,发育含灰云坪、灰云坪、含泥云坪、泥云坪、云泥坪以及含泥含灰云坪微相,蒸发台地主要分布于研究区东部,沉积微相类型以含膏云坪和含膏湖为主.马五34小层整体发育局限台地亚相,含泥云坪和泥云坪分布面积最广;马五24小层沉积时期,研究区东部蒸发台地沉积范围略有增加;马五1b4小层沉积时期,陆源泥质输入再次明显增加,中部地区广泛发育泥云坪沉积;马五 小层沉积时期,陆源泥质输入减少,区内广泛发育灰云坪沉积微相,局部地区发育蒸发台地亚相.沉积微相对天然气分布具有明显控制作用,灰云坪和含泥云坪为研究区马五4亚段天然气分布的有利沉积微相.研究成果可以为靖边气田碳酸盐岩储层分布有利区预测及天然气勘探开发方案部署提供科学依据.
Characteristics and evolution of sub-member Ma45 of Majiagou Formation in southern Jingbian gas field,Ordos Basin
As one of the critical replacement production layers following the Sub-member Ma55 of the Ordovi-cian Majiagou Formation in the Jingbian gas field,the sub-member Ma45 is limited in the reasonable and accu-rate prediction for the carbonate reservoir development and natural gas distribution because of the weak analy-sis on the sedimentary microfacies.Taking the southern Jingbian gas field as an example,the sedimentary mi-crofacies type were identified and the planar distribution law was described,and the evolution law of sedimen-tary microfacies of different layers from the sub-member Ma45 was made clear in this paper through core obser-vation,thin section identification and logging interpretation for sedimentary facies.The results show that the sedimentary subfacies of the sub-member Ma45 is dominated by restricted platform in the central and western study area,including lime-bearing dolomite flat,calciferous dolomite flat,mud-bearing dolomite flat,argilla-ceous dolomite flat,dolomitic mud flat,and mud-lime bearing dolomite flat.The evaporation platform is main-ly distributed in the eastern study area,and dominated by gypsiferous dolomite flat and gypsiferous lake.The Ma4-35 layer is dominated by restricted platform,with the largest area of mud-bearing dolomite flat and mud dol-omite flat development.During the sedimentary period of Ma4-25 layer,the evaporation platform area in the east-ern study area increased.The content of terrigenous mud increases again when in the Ma4-1b5 layer sedimentary period resulting in the extensive development of mud dolomite flat in the central study area,while decreases during the Ma4-1a5 layer sedimentary period resulting in the extensive distribution of calciferous dolomite flat de-velopment with local development of evaporation platform.The natural gas distribution is controlled obviously by sedimentary microfacies.The calciferous dolomite flat and mud-bearing dolomite flat are the favorable sedi-mentary microfacies for natural gas distribution of sub-member Ma45 in the study area.The research results is helpful for the prediction of favorable carbonate reservoir distribution areas and the deployment of natural gas exploration and development scheme in Jingbian gas field.

sedimentary microfaciescarbonate rockMajiagou FormationJingbian gas fieldOrdos Basin

李百强、郭艳琴、徐宏杰、吴珍珍、王起琮、张小莉、巨银娟、李文厚

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安徽理工大学地球与环境学院,安徽淮南 232001

西北大学地质学系/大陆动力学国家重点实验室,陕西西安 710069

西安石油大学陕西省油气成藏地质学重点实验室,陕西西安 710065

西安石油大学地球科学与工程学院,陕西西安 710065

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沉积微相 碳酸盐岩 马家沟组 靖边气田 鄂尔多斯盆地

2024

西北大学学报(自然科学版)
西北大学

西北大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.35
ISSN:1000-274X
年,卷(期):2024.54(6)