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cations diffuse through it. Geo-chemical alteration of minerals prone to acid attack, can occur because of the chemical dis- equilibrium between the brine, saturating the clayey rock, and the acidified
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investigate: - Mineralogical transformations—particularly clay mineral alterations—resulting from fluid flow, - Textural relationships between host units, veins, cements, inherited/newly formed minerals
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through the caprock but cations just diffuse through it. Geo-chemical alteration of minerals prone to acid attack, can occur because of the chemical disequilibrium between the brine, saturating the clayey
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