1) solutiontype secondary pores
溶蚀型次生孔隙
1.
The forming mechanism of solutiontype secondary pores is one of the problems which petroleum geologist are very much interested in.
溶蚀型次生孔隙是碎屑岩储集层的一种重要孔隙类型，溶蚀型次生孔隙的形成机制是石油地质学家很感兴趣的问题之一。
2) secondary dissolution pore
次生溶蚀孔隙
1.
The organic reef and bank facies, widely developed in Middle Ordovician Yijianfang Formation in Tahe oilfield , are characterized by point reefs and banks within the caronate platforms, and the reservoir spaces are mainly of microfissures and secondary dissolution pores.
塔河油田中奥陶统一间房组广泛发育的生物礁滩相具有台地内部的点礁、点滩性质,储层的储集空间主要是微裂缝一次生溶蚀孔隙。
4) vugular-solution porosity
溶蚀孔隙度
5) type of secondary pore
次生孔隙类型
6) secondary pores
次生孔隙
1.
Effectiveness of thermochemical sulfate reduction on oil and gas industry—a H_2S formation accelerating development of the secondary pores in reservoirs;
TSR(H_2S)对石油天然气工业的积极性研究——H_2S的形成过程促进储层次生孔隙的发育
2.
Distribution and genesis of secondary pores in Tertiary clastic reservoir in Southwestern Qaidam Basin;
柴西南地区第三系碎屑岩储集层次生孔隙分布及成因
3.
Genesis of heterogeneity of secondary pores in deep reservoir of Jiangling Depression;
江陵凹陷深层储层次生孔隙非均质性成因
补充资料：孤峰溶蚀平原
孤峰溶蚀平原是指峰林平原进一步发育，峰林不断溶蚀降低，地表夷平，仅有少量山峰存在所形成的平原
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