High 18 O ore-forming fluids in volcanic-hosted base metal massive sulfide deposits; geologic, 18 O/ 16 O, and D/H evidence from the Iberian pyrite belt; Crandon, Wisconsin; and Blue Hill, MaineJ. Munhá, R. Kerrich, Fernando Barriga|Economic Geology|1986Cited by 61
Extreme 18O-enriched volcanics and 18O-evolved marine water, Aljustrel, Iberian Pyrite Belt: transition from high to low Rayleigh number convective regimesFernando Barriga, R. Kerrich|Geochimica et Cosmochimica Acta|1984Cited by 43