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