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Stable Isotope and Geochemistry

Carbonate geochemistry utilizes the chemistry and fabric of carbonate minerals to reconstruct the conditions present in ancient environments Stable isotopic and elemental chemistry of carbonate captures a record of the temperature and chemistry of fluid from which it was formed. As such, carbonate chemistry in combination with petrography serves as a important proxy for deciphering the diagenetic changes that control porosity development in reservoirs.

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