Fluids responsible for the deposition of metamorphogenic barite bodies at the Pollone deposit (Apuane Alps, Tuscany, Italy) scarcely interacted with host-rocks, suggesting that they formed in a different reservoir. Remobilization of earlier, sungenetic barite orebodies by synmetamorphic fluids was apparently minor.

O-isotope and geochemical constraints on metamorphogenic barite vein formation at Pollone, Apuane Alps, Tuscany / Costagliola P.; Benvenuti M.; Lattanzi P.; Tanelli G.. - STAMPA. - (1993), pp. 13-14. (Intervento presentato al convegno Final Meeting of IGCP Project No. 291 on "Metamorphic fluids and mineral deposits" tenutosi a Prague (CZ) nel 12-13 July, 1993).

O-isotope and geochemical constraints on metamorphogenic barite vein formation at Pollone, Apuane Alps, Tuscany

COSTAGLIOLA, PILARIO;BENVENUTI, MARCO;LATTANZI, PIERFRANCO;TANELLI, GIUSEPPE
1993

Abstract

Fluids responsible for the deposition of metamorphogenic barite bodies at the Pollone deposit (Apuane Alps, Tuscany, Italy) scarcely interacted with host-rocks, suggesting that they formed in a different reservoir. Remobilization of earlier, sungenetic barite orebodies by synmetamorphic fluids was apparently minor.
1993
Proceedings of the Final Meeting of IGCP Project No. 291 on "Metamorphic fluids and mineral deposits"
Final Meeting of IGCP Project No. 291 on "Metamorphic fluids and mineral deposits"
Prague (CZ)
12-13 July, 1993
Costagliola P.; Benvenuti M.; Lattanzi P.; Tanelli G.
4b - Riassunto in atti di congresso
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Utilizza questo identificatore per citare o creare un link a questa risorsa: https://hdl.handle.net/2158/647424
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