Steeply inclined and filling type of karst fissure-water bearing structure occurred in a steeply inclined angle of fissure, easily accumulate water and form a high water pressure in its fissure space.
高陡倾充填型岩溶裂隙蓄水构造呈高角度裂缝状产出，降雨后，极易在其裂隙空间内积水形成高水压；
Steeply inclined and filling type of karst fissure-water bearing structure occurred in a steeply inclined angle of fissure, easily accumulate water and form a high water pressure in its fissure space.
高陡倾充填型岩溶裂隙蓄水构造呈高角度裂缝状产出，降雨后，极易在其裂隙空间内积水形成高水压；
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