松辽盆地北部深部储层的次生孔隙发育机制和控制因素  

Generation Mechanism of Secondary Porosity and Control Factors in Deep Sandstone Hydrocarbon Reservoirs, Northern Songliao Basin

作　　者：杨宝星[1] 李南豪[1] 古世祥 

机构地区：[1]成都地质学院 [2]大庆石油管理局

出　　处：《沉积学报》1991年第4期34-42,共9页Acta Sedimentologica Sinica

摘　　要：本文对研究区内的次生溶孔的形成机制和控制因素进行了探讨:1.次生格架颗粒溶孔和粒间溶蚀扩大孔的形成机制:一是主要与沉积间断,即表生期地表淡水渗入有关的溶蚀作用机制;另一种是与埋藏期泥岩中有机质成熟作用有关的格架颗粒溶孔发育的机制.2.浊沸石溶孔的形成机制:有机质进入高成熟阶段,烃类热裂解造成孔隙水的pH值降低,并产生少量二氧化碳,导致浊沸石的溶解.沉积间断的存在和土壤化作用、泥岩中有机质的丰度和干酪根类型是控制次生孔隙发育的主要因素.据此对储层进行了区域性评价。Songliao Basin formed by rifting in craton interior during the Yanshan Movement of Late Jurassic. The deep stratigraphy of Songliao Basin includes the Upper Jurassic (J2-3) and the Lower Cretaceous formations (K1d & K1q1-2). The succession consisting mainly of sandstone, shale and coal-bearing sequence and partially volcanics, volcaniclastic rocks were established during the rifting and the early depression stage. The clastic sequence displays terrestrial alluvial fan, fan delta, fluvial floodplane and lacustrine sedimentary facies. The sandstone reservoirs are mineralogically characterized by immature feldspathic litharenite and lithic arkose and have been altered by a series of diagenetic alteration. The secondary dissolution pores are frequently found as the dominant type of porosity including framework dissolution porosity, intergranular dissolution enhanced porosity and authigenetic laumontite dissolution porosity. This paper describes the dissolution mechanism and its control factors. The effect of organic acids on dissolution of aluminosilicate is closely taken into account since many information of organic-inorganic interaction and sandstone porosity enhancement have been demonstrated in recent years. 1. The generation mechanism of framework grain dissolution porosity and intergranular dissolution enhanced porosity. Two types of mechanism are suggested based on the distribution and association of these dissolution pores. One is related to the telogenetic percolating meteoric water in correspondence with the sedimentary hiatus during the end of K,d stage. As the result, porosity are largely by combinning the intergranular dissolution enhanced porosity and detrital grain dissolution porosity. The generation mechanism of framework grain dissolution porosity could be basically contributed to the maturation of type Ⅲ kerogen in the Jurassic coal-bearing sequence. Carbonic acid and short-chain aliphatic acid effectively provides H+ and Al-complexing agent to the pore solution. Thus this type

关 键 词：烃 储集层 次生孔隙 发育机制 

分 类 号：P618.130.2[天文地球—矿床学]