溶蚀作用使石灰石路面的灰岩深沟变宽变深。
Solutional processes have widened and deepened the grykes of the limestone pavement.
破裂作用可以提高砂岩的储渗能力,同时也有利于砂岩中溶蚀孔隙的形成。
Fracturing has resulted in an increase in sandstone porosity and permeability and enhanced the development of secondary pores.
原生裂缝是岩浆冷凝结晶过程中形成的裂缝; 次生裂缝是火山岩及其原生裂缝系统受后期构造运动、溶蚀、风化等作用改造而形成的裂缝。
Primary fracture were formed during the lava crystal and the secondary fracture generated during the volcanic reconstruction by tectonic movement, and wind action, solution.
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