Current knowledge of sulphur, carbon and oxygen isotope systematics of synmetamorphic ore deposits from the Apuane Alps region (Tuscany, Italy) is presented here. Results indicate that ore-forming fluids of metamorphic nature intensely interacted and isotopically equilibrated with basement rocks, leaching metals and other elements and depositing them in structurally-controlled sites under favourable P(f conditions.
A genetic model of polymetallic ore deposits from Apuane Alps: evidences from stable isotope data / Benvenuti M.; Costagliola P.; Lattanzi P.; Cortecci G.; Tanelli G.. - STAMPA. - (1991), pp. 249-252. (Intervento presentato al convegno 25th years SGA Anniversary Meeting tenutosi a Nancy (France) nel 30 August-3 September 1991).
A genetic model of polymetallic ore deposits from Apuane Alps: evidences from stable isotope data
BENVENUTI, MARCO;COSTAGLIOLA, PILARIO;LATTANZI, PIERFRANCO;TANELLI, GIUSEPPE
1991
Abstract
Current knowledge of sulphur, carbon and oxygen isotope systematics of synmetamorphic ore deposits from the Apuane Alps region (Tuscany, Italy) is presented here. Results indicate that ore-forming fluids of metamorphic nature intensely interacted and isotopically equilibrated with basement rocks, leaching metals and other elements and depositing them in structurally-controlled sites under favourable P(f conditions.
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