溶解孔隙，简称溶孔。因溶解作用而产生的孔隙。是岩石中最多也是最重要的次生孔隙类型之一,包括岩石的可溶性颗粒、基质、胶结物和交代物被溶解产生的孔隙,从泛指的角度上也包括被溶解改造的各种裂隙。碎屑岩中,最普遍且最有意义的是粒间和胶结物内的溶解孔隙。
... solution polymerization 溶液聚合 solution porosity 溶解孔隙 solution pressure 溶解压；溶解压强 ...
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岩溶空隙系统虽然在形成后又被充填，但为埋藏溶解孔隙的发育提供了条件。
Although karst pore system was packed again after forming, it provides conditions for the development of burial corrasion pores.
储集空间以溶解孔隙和裂缝为主，裂缝主要有构造裂缝、压实裂缝和解理裂缝；
There exist two chief types of reservoir space: the one is fractures including structural fractures, compaction fractures and cleavage cracks;
而碳酸盐的溶解作用形成了大量次生孔隙空间，增加了砂岩的孔隙度。
The porosity increasing is primarily due to the resolution of carbonate so that a large amount of the secondary pore space is resulted.
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