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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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A study of the general features of the vapor pressures of hydrous materials indicates that thermal gradients in wet sediments may be influenced by endothermic dehydration reactions. Stress and salinity may influence the temperature of dehydration. The large solubility of stressed grains must lead to rapid elimination of porosity and to the condition that fluid pressures approach lithostatic pressures during sinking of wet sediments.
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