Retrogressive fluids and vein formation during uplift of the Priestley metamorphic complex, north Victoria Land, Antarctica

The poly-deformed Priestley schist (Wilson Terrane) of north Victoria Land, Antarctica ranges in metamorphic grade from lower greenschist facies to upper amphibolite facies. All grades of schist have been affected by structurally controlled retrogressive H 2 O-CO 2 fluids with 45–70 mole % CO 2 . Th...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Craw, D., Cook, Y.A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1995
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102095000393
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102095000393