高级检索
    苏奥, 陈红汉, 詹海勇, 杨文帅, 王存武. 东海西湖凹陷西斜坡和西次凹近致密-致密砂岩气藏的地质特征及发育前景[J]. 中国地质, 2015, 42(4): 1115-1125.
    引用本文: 苏奥, 陈红汉, 詹海勇, 杨文帅, 王存武. 东海西湖凹陷西斜坡和西次凹近致密-致密砂岩气藏的地质特征及发育前景[J]. 中国地质, 2015, 42(4): 1115-1125.
    SU Ao, CHEN Hong-han, ZHAN Hai-yong, YANG Wen-shuai, WANG Cun-wu. Development prospects and geological characteristics of nearly tight and tight sandstone gas reservoirs in western secondary sag and western slope zone of Xihu depression, East China Sea[J]. GEOLOGY IN CHINA, 2015, 42(4): 1115-1125.
    Citation: SU Ao, CHEN Hong-han, ZHAN Hai-yong, YANG Wen-shuai, WANG Cun-wu. Development prospects and geological characteristics of nearly tight and tight sandstone gas reservoirs in western secondary sag and western slope zone of Xihu depression, East China Sea[J]. GEOLOGY IN CHINA, 2015, 42(4): 1115-1125.

    东海西湖凹陷西斜坡和西次凹近致密-致密砂岩气藏的地质特征及发育前景

    Development prospects and geological characteristics of nearly tight and tight sandstone gas reservoirs in western secondary sag and western slope zone of Xihu depression, East China Sea

    • 摘要: 提要:基于沉积构造背景和大量钻测资料,利用气样地球化学测试、铸体薄片、扫描电镜、激光扫描共聚焦显微镜和阴极发光等手段,揭示了东海西湖凹陷西斜坡和西次凹近致密-致密砂岩气藏的地质特征,并分析了发育前景。研究结果表明:2个靶区近致密-致密砂岩气藏均分布在中深层,且位于常规气藏之下,但发育层位不同,西斜坡在平湖组中下段,西次凹在花港组下段。2个靶区的近致密-致密砂岩气均为煤型气,来源于平湖组煤系源岩,西次凹致密气藏属于“下生上储”型,西斜坡属于“自生自储”型。西次凹属于典型的致密砂岩储层,西斜坡属于近致密砂岩储层。强压实作用和硅质、自生伊利石及碳酸盐胶结是储层致密化的重要因素。溶孔和原生粒间孔是致密砂岩储层主要储集空间;2个靶区的近致密-致密储层不同深度段发育“孔隙型”甜点,为酸性溶蚀成因,但西斜坡的溶蚀强度大于西次凹。另外,西次凹深层发育部分裂缝,形成该区“裂缝型”甜点。西次凹致密气藏具有弱超压特征,西斜坡具有超压-强超压特征。平湖组广覆式分布高有机质丰度的煤系源岩全天候持续供气是靶区发育大规模近致密-致密砂岩气藏的物质基础,大面积近致密-致密储层提供了良好的储集体,因此发育前景好,勘探潜力大。

       

      Abstract: Abstract: Based on tectonic and sedimentary background as well as a large number of drilling and logging data, the authors studied geological characteristics and development prospects of nearly tight and tight sandstone oil and gas reservoirs in western secondary sag and western slope zone of Xihu depression, East China Sea by using casting thin section, laser scanning confocal microscope, scanning electron microscope, cathodoluminescence, stable carbon isotope composition and light hydrocarbon components. The results indicate that nearly tight and tight sandstone gas reservoirs are distributed under the conventional gas reservoir, but their development horizon are different, belonging respectively to middle and lower Pinghu Formation and lower Huagang Formation. Nearly tight and tight sandstone gas is coal-type gas and came from coal measures source rock in Pinghu Formation. The reservoir is above source rock in western secondary sag, and multiple reservoir and source rock are superimposed upon each other in western slope zone. Western secondary sag reservoir belongs to tight sandstone and western slope zone reservoir is nearly tight sandstone. Strong compaction, siliceous cement, authigenic illite cementation and carbonate cementation are important factors for densification of the reservoir. The pore types of two zones mainly include intergranular dissolved pore, native intergranular pore and feldspar intragranular dissolved pore. There are relatively high porosity and high permeability reservoirs in different depths of the two zones, resulting from acid dissolution. However, western slope zone reservoir has larger corrosion scale and does not develop microfracture. There is a certain size of microfracture which is “microfracture” sweet spot in deep layer of western secondary sag. The former has weak overpressure and the latter has overpressure-strong overpressure. The source rocks which have high abundance of organic matter in Pinghu Formation are distributed widely in Xihu depression. The supply of continuous gas constitutes the material basis of large-scale development of nearly tight and tight sandstone gas reservoirs. Large-sized nearly tight and tight sandstone provides effective reservoirs. So, there are rich tight sandstone oil and gas resources in East China Sea.

       

    /

    返回文章
    返回