ISSN 1673-8217 CN 41-1388/TE
主管:中国石油化工集团有限公司 主办:中国石油化工股份有限公司河南油田分公司
陈建文, 张晓博, 韩詹, 曾凤凰, 王玥, 朱玉双. 2020: 鄂尔多斯盆地合水地区长2_3沉积相及储层非均质性研究. 石油地质与工程, 34(02): 61-65.
引用本文: 陈建文, 张晓博, 韩詹, 曾凤凰, 王玥, 朱玉双. 2020: 鄂尔多斯盆地合水地区长2_3沉积相及储层非均质性研究. 石油地质与工程, 34(02): 61-65.
CHEN Jianwen, ZHANG Xiaobo, HAN Zhan, ZENG Fenghuang, WANG Yue, ZHU Yushuang. 2020: Sedimentary facies and reservoir heterogeneity of Chang 2_3 in Heshui area of Ordos basin. Petroleum Geology and Engineering, 34(02): 61-65.
Citation: CHEN Jianwen, ZHANG Xiaobo, HAN Zhan, ZENG Fenghuang, WANG Yue, ZHU Yushuang. 2020: Sedimentary facies and reservoir heterogeneity of Chang 2_3 in Heshui area of Ordos basin. Petroleum Geology and Engineering, 34(02): 61-65.

鄂尔多斯盆地合水地区长2_3沉积相及储层非均质性研究

Sedimentary facies and reservoir heterogeneity of Chang 2_3 in Heshui area of Ordos basin

  • 摘要: 鄂尔多斯盆地合水地区是近年来重要的勘探区域,研究储层非均质性特征可为生产提供更多的科学依据。为了研究合水地区延长组长2_3储层的非均质性,在小层精细划分与对比的基础上,利用钻井岩心、测井及分析测试等资料,通过层内非均质性、层间非均质性、平面非均质性三个方面研究长2_3储层的非均质性特征。结果表明,长2_3储层的非均质性与沉积相带关系密切,研究区为三角洲前缘亚相沉积,分流间湾、水下天然堤等微相的孔隙度和渗透率相对较低,水下分流河道微相和砂体厚度较大的有利沉积相带的孔隙度和渗透率都逐渐变大,高孔高渗带大都重合,即高孔带为对应的高渗带,沉积相带对储层非均质性有明显的控制作用。

     

    Abstract: Heshui area of Ordos basin is an important exploration area in recent years, and the study of reservoir heterogeneity can provide more scientific basis for production. In order to make clear the heterogeneity of Yanchang 2_3 reservoir in Heshui area, based on the fine division and correlation of small layers, the heterogeneity characteristics of chang2_3 reservoir are studied by using drilling core, well logging, analysis and testing data, through three aspects of heterogeneity in layers, between layers and on the plane. The results show that the heterogeneity of Chang 2_3 reservoir is closely related to the sedimentary facies zone. The study area belongs to delta front sub facies deposition, and the porosity and permeability of microfacies such as distributary bay and underwater natural levee are relatively low, while the porosity and permeability of underwater distributary channel microfacies and the favorable sedimentary facies zone with larger thickness of sand bodies are gradually increasing, that is to say, the high porosity zone is right the high permeability zone, and the sedimentary facies zone plays an important role in controlling the reservoir heterogeneity.

     

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