Extreme 18O-enriched volcanics and 18O-evolved marine water, Aljustrel, Iberian Pyrite Belt: transition from high to low Rayleigh number convective regimes-Reference-Cited by-同舟云学术

Extreme 18O-enriched volcanics and 18O-evolved marine water, Aljustrel, Iberian Pyrite Belt: transition from high to low Rayleigh number convective regimes

Published:1984-05 Issue:5 Volume:48 Page:1021-1031
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Barriga F.J.A.S,Kerrich R

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference90 articles.

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3. Metamorphism and massive sulphide generation in oceanic crust;Andrews;Geosci. Can.,1976

4. Hydrothermal metamorphism and ore genesis at Aljustel, Portugal;Barriga,1983

5. High 18O fluids, circulation regimes and mineralization at Aljustrel, Iberian Pyrite Belt;Barriga;Geol. Soc. Amer. Abs. W. Pgs.,1981

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