石炭系印支期的古构造高部位是埋藏溶解孔发育的有利地区。
The palaeostructure high part of Carboniferous in Indosinian epoch is favourable to the development of burial corrasion pores.
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.
其中建设性成岩作用主要是表生岩溶作用、埋藏溶解作用，破坏性成岩作用主要为各期的充填作用，对孔隙破坏性最大的胶结物是亮晶方解石。
The constructive diagenesis are mainly epigenic karstification and burial dissolution. The destructive diagenesis are filler in each periods, the most devastating cement to porous is sparry calcite.
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