Abstract
Drawing on the results of a great number of studies , this paper aims to make apparent a rationale of the various processes and their interactions in gypsum karst and associated evaporites. They include the effect of diapirism, dissolution and chain reactions, cave collapse and external geomorphic processes. In the case of cave formation, the paper underlines the role of aquifers in wall and roof layers.
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More From: Karstologia : revue de karstologie et de spéléologie physique
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