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付行, 杜学斌, 徐国盛, 梁家驹, 丁圣斌. 东海宁波构造带深层花港组砂岩储层致密性特征及控制因素[J]. 海洋石油, 2018, 38(1): 1-8. DOI: 10.3969/j.issn.1008-2336.2018.01.001
引用本文: 付行, 杜学斌, 徐国盛, 梁家驹, 丁圣斌. 东海宁波构造带深层花港组砂岩储层致密性特征及控制因素[J]. 海洋石油, 2018, 38(1): 1-8. DOI: 10.3969/j.issn.1008-2336.2018.01.001
FU Hang, DU Xuebin, XU Guosheng, LIANG Jiaju, DING Shengbin. Characteristics and Controlling Factors of Tight Sandstone Reservoir of Huagang Formation in the Ningbo Tectonic Belt of Xihu Sag[J]. Offshore oil, 2018, 38(1): 1-8. DOI: 10.3969/j.issn.1008-2336.2018.01.001
Citation: FU Hang, DU Xuebin, XU Guosheng, LIANG Jiaju, DING Shengbin. Characteristics and Controlling Factors of Tight Sandstone Reservoir of Huagang Formation in the Ningbo Tectonic Belt of Xihu Sag[J]. Offshore oil, 2018, 38(1): 1-8. DOI: 10.3969/j.issn.1008-2336.2018.01.001

东海宁波构造带深层花港组砂岩储层致密性特征及控制因素

Characteristics and Controlling Factors of Tight Sandstone Reservoir of Huagang Formation in the Ningbo Tectonic Belt of Xihu Sag

  • 摘要: 西湖凹陷宁波构造带花港组为一套致密砂岩含气储层,研究该储层的致密性及其主控因素对进一步的勘探开发具有重要的意义。基于前人研究成果,以镜下薄片观察资料和测井资料为基础,对花港组储层岩石学特征、物性特征、成岩作用及其主控因素进行了一系列的研究,认为花港组砂岩是典型的低孔低渗—特低孔特低渗储层。岩石类型为长石岩屑质石英砂岩;次生孔隙为主要储集空间。控制储层致密性的主要因素为压实和胶结作用,数学地质模型显示80%以上的孔隙损失与压实作用有关,胶结作用的平均减孔率为7%。

     

    Abstract: The Huagang Formation in Ningbo tectonic belt of Xihu Sag is a set of tight sandstone gas reservoir. The study on the compactness of the reservoir and its main controlling factors is signifcant to further exploration and development. Based on some of the previous researches, thin section analysis and geochemical parameters of core samples, the author studied the petrologic characteristics, physical property, diagenesis and controlling factors for the tight sandstone reservoir of Huagang Formation. It's believed that the Huagang Formation sandstone is a typical low porosity and low permeability and ultra-low porosity and permeability reservoir. The rock type is feldspathic lithic quartz sandstone, and the secondary porosity is the main reservoir space. The main factors controlling the compactness of the reservoir are compaction and cementation. The mathematical geology model shows that more than 80% of the pore loss are related to compaction, and the average pore reduction rate of cementation is 7%.

     

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