In this work we have attempted to reconstruct hornblende-forming mineral reactions in oceanic lower-crust gabbro to trace the magmatic/hydrothermal transition and to constrain temperature, pressure, oxygen fugacity, and fluid composition for the reaction zone. The results are based on mineral chemistry including trace elements, study of fluid inclusions and thermodynamic calculations.
Reducing reactions of hydrothermal front in lower-crustal magmatically active zone: an example from the Vema lithospheric section, central Atlantic / Pertsev, A.; Cipriani, Anna; Aranovich, L.; Prokofiev, V.. - (2012), p. 1401. (Intervento presentato al convegno 34th International Geological Congress tenutosi a Brisbane, Australia. nel 5-10 August 2012).
Reducing reactions of hydrothermal front in lower-crustal magmatically active zone: an example from the Vema lithospheric section, central Atlantic
CIPRIANI, Anna;
2012
Abstract
In this work we have attempted to reconstruct hornblende-forming mineral reactions in oceanic lower-crust gabbro to trace the magmatic/hydrothermal transition and to constrain temperature, pressure, oxygen fugacity, and fluid composition for the reaction zone. The results are based on mineral chemistry including trace elements, study of fluid inclusions and thermodynamic calculations.
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