基于成岩相划分的低渗透储层有利区预测 ——以陆丰凹陷文昌组砂岩储层为例
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戴建文(1983—),男,江西抚州人,高级工程师,硕士,从事油田开发地质研究、开发方案编制及项目管理工作。E-mail:daijw2@cnooc.com.cn。

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国家科技重大专项“南海东部油田上产2000 万吨关键技术研究”课题5“深层古近系油藏高效开发技术研究”(CNOOC-KJ 135ZDXM 37 SZ 05 SZ)。


Prediction of favorable zones in low-permeability reservoirs based on diagenetic facies delineation: A case study of sandstone reservoirs of Wenchang Formation in Lufeng Sag
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    摘要:

    珠江口盆地LF14 含油构造的发现揭示了陆丰凹陷文昌组具有巨大的油气勘探潜力,但勘探实践揭示相同沉积相带的砂体物性差异极大,成岩作用对储层物性的影响作用尚不明确,制约了研究区优质储层预测。为实现低渗透储层有利区预测,基于薄片鉴定、扫描电镜、X-射线衍射、物性测试等分析测试手段,结合钻井资料,对陆丰凹陷文昌组砂岩储层展开成岩相研究,并通过成岩相划分完成研究区低渗透储层有利区预测。结果表明,文昌组储层主要发育石英砂岩,成分成熟度、结构成熟度均较高,储集空间以粒间溶孔为主。研究区识别出中压实弱胶结强溶解、强压实中胶结中溶解、中压实强胶结弱溶解、强压实中胶结弱溶解4 类成岩相。其中中压实弱胶结强溶解相为研究区最有利成岩相,多发育在水下分流河道;强压实中胶结中溶解相的物性次之,主要发育在河口坝;中压实强胶结弱溶解相及强压实中胶结弱溶解相为非有利成岩相。垂向上,基于测井资料,利用岩石物理参数、物性参数对储层成岩相类型进行了综合识别;平面上,通过成岩相与地震波阻抗及泊松比的相关性分析,发现中压实弱胶结强溶解相、强压实中胶结中溶解相的泊松比较低,而非有利成岩相泊松比偏高,在此基础上利用泊松比反演结果在研究区开展低渗透储层有利区预测。

    Abstract:

    The discovery of LF14 oil-bearing structure in Pearl River Mouth Basin suggests that Wenchang Formation in Lufeng Sag has significant potential for oil and gas exploration. However, exploration practice reveals that the physical properties of sand bodies in the same sedimentary facies belt vary greatly. The influence of diagenesis on the physical properties of reservoirs is not clear, which restricts the prediction of high-quality reservoirs in the study area. In order to predict the favorable zones in lowpermeability reservoirs, the diagenetic facies of sandstone reservoirs of Wenchang Formation in Lufeng Sag was studied based on thin section identification, scanning electron microscopy, X-ray diffraction, and physical property testing, along with drilling data.The favorable zones in low-permeability reservoirs in the study area were predicted by diagenetic facies delineation. The results show that reservoirs of Wenchang Formation primarily consist of quartz sandstone, which has a high degree of maturity in composition and structure. The reservoir space is characterized by interparticle dissolution pores. Four distinct diagenetic facies are identified in the study area, including moderate compaction-weak cementation-strong dissolution, strong compaction-moderate cementationmoderate dissolution, moderate compaction-strong cementation-weak dissolution, and strong compaction-moderate cementationweak dissolution. Among these facies, the moderate compaction-weak cementation-strong dissolution is the most favorable facies in the study area, with the majority of the facies occurring in the underwater distributary channels. The strong compaction-moderate cementation-moderate dissolution has the second most favorable physical properties and is mainly developed in the mouth bars. The moderate compaction-strong cementation-weak dissolution and the strong compaction-moderate cementation-weak dissolution are unfavorable diagenetic facies. Vertically, the diagenetic facies types of the reservoirs are comprehensively identified based on well logging data by utilizing petrophysical parameters and physical properties. Laterally, through the analysis of the correlation among diagenetic facies, seismic acoustic impedance, and Poisson’s ratio, it was found that the moderate compaction-weak cementationstrong dissolution and the strong compaction-moderate cementation-moderate dissolution have relatively low Poisson’s ratios,while unfavorable diagenetic facies have relatively high Poisson’s ratios. On this basis, Poisson’s ratio inversion results are used to predict the favorable zones in low-permeability reservoirs in the study area.

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戴建文,王华,涂乙,朱锐,杨娇,蒋庆平,代云娇,司振宇.基于成岩相划分的低渗透储层有利区预测 ——以陆丰凹陷文昌组砂岩储层为例[J].油气地质与采收率,2025,32(1):40~52

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  • 收稿日期:2024-07-30
  • 最后修改日期:2024-11-30
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  • 在线发布日期: 2025-02-13
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