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.I documenti in FLORE sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.