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Hypogenic caves in Provence (France): Specific features and sedimentsKeywords: hypogenic karst , hydrothermalism , subaqueous calcite deposits , condensation corrosion Abstract: Two dry caves from French Provence (Adaouste and Champignons caves) were until now considered as “normal” caves, evolved under meteoric water flow conditions. A new approach gives evidence of a hypogenic origin from deep water uprising under artesian conditions. Specific morphologies and sediments associated with this hydrology are discussed.
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