摘要
本文探讨了陆1井岩屑砂岩的成岩作用及其对砂岩储层的影响.研究表明,压实作用使岩屑砂岩的孔隙度随埋深迅速减小,成岩早期的胶结物使大部分原生孔隙被充填。水化作用在成岩早期及有机质半成熟和成熟期成岩作用过程中,制约着各个阶段的成岩作用特点。在水化作用和有机质热演化作用的共同影响下,使得方解石胶结物发生选择性溶蚀形成了深部(上乌尔禾组)次生孔隙发育带。
The present paper mainly studies the diagenesis and its influence on reservoir property of lithic sandstone which is little studied in China. Reservoir rock of well Lu-1 is terrigenous lithic sandstone including a lot of pyroclastic rock fragments. Porosity and permeability of reservoir reduce swiftly with the increase of burial depth, but there is an abnormal increase of porosity at the depth of 3750-4300m. There are four main pore
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types of sandstone: primary intergranular pores, inner grains dissoluted pores and micropores. Diagenesis and Sedimentary facies are the two main factors affecting reservoir property of well Lu- 1, but the influence of the latter is not very obvious. The diagenetic influence on reservoir property of sandstone is signifcant and has its particularity to this kind of low mature lithic sandstone of well Lu-1.
Compaction and hydration, especially hydration, are the two most important factors which let to the swiftly reduce of porosity, cementation is another important factor of making porosity and permeability worse. Cements of sandstone are calcite, quartz, authigenic clay, zeolite and a little terrigenous matter. Selective dissolution of calcite cement is the main reason which made the porosity and permeability of partial section better. The influence of calcite replacement on porosity and permeability is not valuable.
The formation of seceondary dissolution pore is related to CO2 which formed by evolution of organic matter. CO2 can be formed during the whole maturation process especially in stage 'A'. Generally, the developing belt of secondary pore is in the early period of 'A',however, calcite cement in this period hasn't any trace of dissolution in well Lu-1, on the contrary, a lot of elastics are replaced by calcite. Selective dissolution of calcite hasn't take place until late period of 'A' and early period of 'B'. The reason is that; during early period of 'A', under alkalline diagenetic environment formed by hydration, the action of CO2 is favourable to the precipitation of calcite, and made replacement developed, but in late period of 'A' and early period of 'B'. hydration nearly disappeared and the neutralization of CO2 changed pores into weak acidity (there is a little CO2 in this period), selective dissolution of calcite cement can be taken place then the belt of secondary pore was formed.
出处
《沉积学报》
CAS
CSCD
北大核心
1991年第4期69-77,共9页
Acta Sedimentologica Sinica
