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Role of fluid mixing in deep dissolution of carbonates

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dc.creator Corbella, M.
dc.creator Ayora, Carlos
dc.date 2007-12-03T12:12:29Z
dc.date 2007-12-03T12:12:29Z
dc.date 2003-12
dc.date.accessioned 2017-01-31T00:59:16Z
dc.date.available 2017-01-31T00:59:16Z
dc.identifier Geologica Acta 1 (4): 305-313 (2003)
dc.identifier 1695-6133
dc.identifier http://hdl.handle.net/10261/2473
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2473
dc.description The presence of cavities filled with new minerals in carbonate rocks is a common feature in oil reservoirs and lead-zinc deposits. Since groundwater equilibrates rapidly with carbonates, the presence of dissolution cavities in deep carbonate host rocks is a paradox. Two alternative geochemical processes have been proposed to dissolve carbonates at depth: hydrogen sulfide oxidation to sulfuric acid, and metal sulfide precipitation. With the aid of geochemical modeling we show that mixing two warm solutions saturated with carbonate results in a new solution that dissolves limestone. Variations in the proportion of the end-member fluids can also form a supersaturated mixture and fill the cavity with a new generation of carbonate. Mixing is in general more effective in dissolving carbonates than the aforementioned processes. Moreover, mixing is consistent with the wide set of textures and mineral proportions observed in cavity infillings.
dc.description Part of this research was funded by the Spanish Ministry of Education and Culture through grant DGESIC-PB98-0901. The reactive transport code RETRASO was developed under a contract with ENRESA (Spain).
dc.description Peer reviewed
dc.language eng
dc.publisher Consejo Superior de Investigaciones Científicas (España)
dc.publisher Universidad de Barcelona
dc.rights openAccess
dc.subject Hydrothermal karst
dc.subject MVT deposits
dc.subject Reactive transport
dc.subject Fluid mixing
dc.subject Carbonate dissolution
dc.title Role of fluid mixing in deep dissolution of carbonates
dc.type Artículo


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