1) reservoir space
储集空隙
2) water storing void
储水空隙
3) concentrated voids
密集空隙
4) K-lacunary set
K-空隙集
1.
For the integrality of this paper, we prove in appendix that (K,R)-lacunary set and (K,L)-lacunary set are particular cases of the K-lacunary set defined in [6].
为了本文的完整性,在附录中我们证明了(K,R)-空隙集和(K,L)-空隙集是[6]中定义的K-空隙集的特例。
5) lacunary set
空隙集
1.
Using mathematical induction,the relationship between the set identified with K-lacunary tree and K-lacunary set is obtained.
研究K-空隙树的结构,K∈N,利用数学归纳法得到了与K-空隙树对应的数集和K-空隙集的关系。
6) storage space
储集空间
1.
The storage space is dominatecd by the solution micropores, the honeycomb-like solution pores and the kaolinitic intercrystalline pores with small to very small pore throat.
鄂尔多斯盆地北部塔巴庙地区上古生界发育一套低孔低渗致密砂岩储层 ,储集空间以溶蚀微孔、蜂窝状溶孔和高岭石晶间隙为主 ,孔喉以细—微细为主。
2.
The storage spaces of the carbonate rocks resulted from the interaction of multistage dissolution and infilling,which may be divided into four stages on the basis of the development and evolution.
陕甘宁盆地中部气田产于奥陶系顶部古风化壳碳酸盐岩储集体中，碳酸盐岩储集空间的形成是不同期次的溶蚀作用和充填作用相互作用的结果。
3.
In-depth analysis is made on lithology,storage space type,porosity evolution,pore-fissure combination of volcanic rocks and their influencing factors in northwestern margin of Junggar basin.
对准噶尔盆地西北缘火山岩岩性特征、储集空间类型、孔隙演化、孔缝组合类型及其主要影响因素进行了深入分析,研究了区内6种火山岩的岩性特征和6种类型储集空间特征及形成机理,认为火山岩原生孔隙因连通性差而不能形成有效储集层,而经过后期改造作用,尤其是溶蚀作用和构造运动,将大大改善火山岩的储集性能而成为有效储集层。
补充资料：储层描述(见油气田储层评价)
储层描述(见油气田储层评价)
reseroir evaluation of oil and gas field
储层描述(reseroir evaluation of 011 and gasfield)见油气田储层评价。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条