Underground Karstification in Saturated Water.

被引：0

作者：

Briffoz, Albert ^{[1
]}

Ek, Camille ^{[1
]}

Gewelt, Michel ^{[1
]}

机构：

[1] Rue de Dolembreux 7, B-4050 Esneux, Belgium.

来源：

Annales de la Societe Geologique de Belgique | 1984年 / 108卷

关键词：

FLOW OF WATER - Underground - GEOLOGY - Caves - HYDROLOGY - WATER; UNDERGROUND - Corrosive Effects;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

In order to explain the development of caves, considering the slowness of water circulation into the fissures of the limestone, only a chemical action i. e. corrosion can be called upon in most cases. However, as saturation is rapidly reached, we consider, in order to extend the dissolution action of underground water, the possibility of dissolution in a saturated environment.

引用

页码：251 / 254

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