首页|鄂尔多斯盆地延113井区山西组沉积微相研究

鄂尔多斯盆地延113井区山西组沉积微相研究

扫码查看
本文综合应用岩心、测井和分析测试等资料,以鄂尔多斯盆地延 113 井区山西组为研究对象,总结了岩石学特征、泥岩颜色、粒度分析、沉积层理等相标志特征,开展了延 113 井区山西组沉积微相类型、特征及沉积相展布规律研究.研究结果表明:研究区整体为三角洲前缘沉积环境,包括水下分流河道和分流间湾两种沉积微相.山 2段水下分流河道呈北东-南西向展布,河道宽广,分布范围大.山 1 段海平面大幅下降,三角洲前缘水下分流河道向南进一步延伸,四条主河道由北往南全区贯通,且河道向南变窄分叉,水下分流河道沉积微相是研究区的主要储集相带.
Sedimentary microphase study of Shanxi formation in Yan 113 well area,Ordos Basin
This paper comprehensively applies the data of core,logging and analytical test-ing,and takes the Shanxi formation in Yan 113 well area of Ordos Basin as the research ob-ject,summarizes the petrological characteristics,mudstone color,grain size analysis,sedi-mentary stratification and other phase signatures,and carries out the research on the type and characteristics of sedimentary microphase and sedimentary phase spreading law of the Shanxi formation in the Yan 113 well area.The results of the study show that the whole study area is a delta front sedimentary environment,including two sedimentary microphases,the underwater diversion channel and the diversion bay.The underwater diversion channel in the Shan 2 section spreads in a north-east-south-west direction,with a wide channel and a large distribution range.As the sea level drops significantly in the Shan 1 section,the un-derwater diversion channels at the front edge of the delta extend further to the south,and the four main channels are connected from north to south,and the channels narrow and bifurcate to the south,and the underwater diversion channel sedimentary microphase is the main reservoir phase zone in the study area.

sedimentary microphaseunderwater diversion channeldelta frontphase sig-nature

孙萌思

展开 >

延安大学石油工程与环境工程学院,陕西延安 716000

沉积微相 水下分流河道 三角洲前缘 相标志

陕西省自然科学基础研究计划项目延安大学博士科研启动项目大学生创新训练计划

2020JQ-798YDBK2018-31D2023123

2024

石油化工应用
宁夏化工学会

石油化工应用

影响因子:0.276
ISSN:1673-5285
年,卷(期):2024.43(9)