Therefore the rock mass structures turn loose.The joints and crannies become the infiltration path for the solution liquid, All these accelerate the dissolution process in the deep part of rock bed.
英
美
释义
岩体密集节理裂隙发育,结构疏松,成为溶蚀液体的入渗通道,加剧深层岩体的溶蚀作用发生。
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