高邮凹陷古近系阜宁组一段沉积特征对储层成岩作用及物性的影响
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国家自然科学基金项目(面上项目,重点项目,重大项目)


The Impact of Sedimentary Characteristics on the Diagenesis and Reservoir Quality of the 1st Member of Paleogene Funing Formation in the Gaoyou Subbasin
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    摘要:

    碎屑岩储层沉积后的物性除受沉积作用影响外,还受到成岩作用改造。但成岩作用是外部动力环境作用于沉积物上发生的,外因通过内因而起作用,因此的成岩作用的演化结果必然受到原始沉积物沉积特征的影响。本次研究通过对高邮凹陷福一顿38口取芯井的岩心描述和400余块样品的普通薄片、铸体薄片和扫描电镜的镜下观察以及物性分析和含油性分析等资料,对储层的岩性、粒度、杂基含量、层理结构、生物扰动构造等因素与储层的成岩现象、物性特征和含油性的关系进行了详细研究,总结了沉积微相对成岩作用、储层物性和含油气的影响。储层的成分对储层的成岩作用及物性有重要影响,岩屑较软,易被压实和溶解,浅埋藏时, 孔隙度和渗透率随着岩屑含量的增大而增大。当埋藏较深时,孔隙度和渗透率随岩屑含量增加而快速下降。储层的粒度对储层的成岩作用及物性也有重要影响,一般随着粒度的增大,孔隙度、渗透率都相应增大。储层的层理类型对成岩作用及物性也有重要影响,块状层理、交错层理或平行层理砂岩的分选性好,杂基含量较低,属于颗粒支撑结构,从而有利于原生孔隙的保存,为后期地下酸性流体对储层的溶蚀改造提供了渗流条件。波状交错层理等砂岩除不具备这一条件外, 砂层内部弯曲的纹层给地下流体的流动增加了困难,不利于次生孔隙的发育和油气的进入。沉积微相对储层物性的控制,主要表现在其对原始物性的控制,分选好、原始物性好的储层在埋藏成岩演化过程中,由于对地层流体的流动的阻力小,其储集空间可以由于致密胶结作用完全消失,也可以得到溶蚀改善和保存。但泥质含量高的储层,其原始物性不好,对地层流体的流动阻力大,尤其是油气难于进入,储层主要遭受破坏,而难以得到改善和保存。

    Abstract:

    In addition to the influence of deposition, physical properties of the clastic reservoirs can be seriesly transformed by diagenesis after deposition. Diagenesis are caused by external dynamic environment acting on the sediment. Because the external causes become operative through internal causes, The diagenetic evolution result are influenced inevitablly by the characteristics of the original sediments. Through the core description of 38 Wells and the observation of ordinary thin section, cast thin section and scanning electron microscope of more than 400 samples, and the analysis of physical properties, the oil bearing properties, the relationships between the factors, like reservoir lithology, grain size, matrix contents, bedding structure, bioturbation structure, and the diagenetic phenomenon, physical properties and oil content are studied in detail. The impact of sedimentary microfacies on diagenesis, reservoir properties and oil and gas are summarized. Composition of the reservoir have an important impact on reservoir diagenesis and physical properties, rock debris is relatively soft, easily compacted and dissolved, during shallow burial, porosity and permeability is increasing with the increasing of rock debris content. When buried deeper, porosity and permeability is decreasing with the rapid increases of the content of rock debris. The granularity of the reservoir also have important impact on the diagenesis and physical properties of the reservoir, generally speaking, porosity and permeability increase according to the increasing of particle size. The bedding types of reservoir also have an important impact on the diagenesis and petrophysical properties, sandstone with massive bedding, cross-bedding, parallel bedding, are with a good sorting and low matrix contents, and have grain support structure, which is conducive to the preservation of primary porosity, which supplied a good seepage conditions for the flow of underground acidic fluid and for the dissolution and alteration to reservoir in latter stage. In sandstone with wavy cross-bedding, in addition to there is not this condition, curved lamina inside sandstone increased the difficulties for underground fluid flow, so it is not conducive to the development of secondary porosity and for the oil and gas to enter. To discuss the controls of sedimentary microfacies to the reservoir properties, is mainly to discuss the control to its original petrophysical properties, during the burial and diagenetic evolution process of good sorted reservoir with high original of petrophysical properties, the resistance to the flow of formation fluids is very low, the reservoir space can completely disappear due to dense cementation, and can be preserved and improved due to the dissolution. Reservoirs with high mud content have a bad original petrophysical properties, and its resistance to the flow of formation fluids is big, especially it is difficult for oil and gas to enter the reservoir, so the reservoir space can hardly be improved and saved, and are mostly be destroyed.

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纪友亮,周勇,刘玉瑞,卢欢,刘启东,王艳艳.2014.高邮凹陷古近系阜宁组一段沉积特征对储层成岩作用及物性的影响[J].地质学报,88(7):1299-1310.
JI Youliang, ZHOU Yong, LIU Yurui, LU Huan, LIU Qidong, WANG Yanyan.2014. The Impact of Sedimentary Characteristics on the Diagenesis and Reservoir Quality of the 1st Member of Paleogene Funing Formation in the Gaoyou Subbasin[J]. Acta Geologica Sinica,88(7):1299-1310.

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  • 收稿日期:2013-04-06
  • 最后修改日期:2013-12-03
  • 录用日期:2013-12-12
  • 在线发布日期: 2014-07-16
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