陕西安塞油田长2和长3储层特征及其非均质性

    Reservoir characteristics and heterogeneity of Chang 2 and Chang 3 oil reservoirs in the Ansai oilfield of Ordos Basin, Shaanxi Province

    • 摘要: 安塞油田长2、长3油层组主要发育辫状河和曲流河沉积,其中河道砂体展布形态受沉积微相控制,呈NE—SW向带状展布,是主要的油气储集层。原生粒间孔和次生粒间溶蚀孔是目的层位的主要孔隙类型,孔喉结构为中小孔—中细喉型及小孔—微喉型,前者为中上等储层,后者为中等储层。储集层孔隙结构和渗透性受成岩事件的影响较大,主要包括机械压实-化学压溶作用、胶结作用和溶蚀作用等。储层孔隙丧失的主要原因是压实、压溶作用和胶结作用,其中,石英、长石次生加大和方解石胶结是造成储层物性降低的主要原因,而包围在碎屑颗粒周围的绿泥石薄膜一方面使粒间孔减小,另一方面阻止了部分石英、长石加大及方解石的沉淀,在一定程度上保存了部分原生粒间孔隙,从而使储层物性较好。表生成岩阶段的大气降水及晚成岩阶段有机质分解形成的酸性流体,是碎屑长石和部分胶结物溶解从而形成大量次生孔隙的主要介质。安塞油田长2和长3油层组在纵向上隔夹层较发育,沉积韵律主要为正反复合韵律,导致了储层较强的非均质性,其中长3油层组较长2油层组非均质性强。

       

      Abstract: There are braid river and meandering river sediments of Chang 2 and Chang 3 oil reservoirs in the Ansai oilfield. The channel sandstone bodies are in NE-SW striking zoning distribution, controlled by sedimentary microfacies, and the sand bodies of river channel are the main reservoirs for the hydrocarbon. Syngenetic open space and vugular-solution pores are main pore types of Chang 2 and Chang 3 oil reservoir sandstones in the Ansai oilfield. Chang 2 and Chang 3 sandstone belongs to the medium or fairly good reservoir whose pore-throat structure belongs mainly to medium-thin throat-eyelet type and thin-small throat- eyelet type. The reservoir quality of the Upper Triassic Chang 2 and Chang 3 sandstones of the Ansai oilfield in Ordos Basin was strongly influenced by the diagenetic events which mainly included mechanical-chemical impaction, consolidation and dissolution.The mechanical-chemical impaction and consolidation were the main factors causing the loss of pores in the sandstones.In the cements,quartz-feldspar overgrowths and carbonate were the main cements that reduced the reservoir quality of the sandstones.Thin chlorite film around detrital grains partially prevented quartz and feldspar overgrowth and carbonate cement precipitation,which caused the preservation of a part of primary pores and hence resulted in a better reservoir quality and the decrease of intergranular space. The main factors for the formation of great quantities of secondary pores were the dissolution of detrital feldspars and part of cements by the meteoric water during epidiagenesis and the acidic liquid related to decomposition of organic mater during hydrocarbon enrichment at the late diagenetic stage. There are many barriers and interbeds in Chang 2 and Chang 3 oil reservoirs, and the sedimentary rhythms are composed of positive rhythms and reverse rhythms which result in the heterogeneity of the competent reservoir, in which the heterogeneity of Chang 3 oil reservoir is stronger than that of Chang 2 oil reservoir in the Ansai oilfield.

       

    /

    返回文章
    返回