Oxygen isotope geochemistry of the Granite Harbour Intrusives, Wilson Terrane, Northern Victoria Land, Antarctica

The oxygen and strontium isotope compositions of the Cambro-Ordovician granitoids cropping out in the Wilson Terrane (Granite Harbour Intrusives-GHI) constrain the petrological evolution of the magmatism in Antarctica, related to the Ross Orogeny. The measured delta(18)O(WR) values of these intrusiv...

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Bibliographic Details
Published in:Mineralogy and Petrology
Main Authors: Dallai L, Ghezzo C, Turi B, Vesica PL
Other Authors: Dallai, L, Ghezzo, C, Turi, B, Vesica, Pl
Format: Article in Journal/Newspaper
Language:English
Published: 2002
Subjects:
Online Access:http://hdl.handle.net/11573/1528769
https://doi.org/10.1007/s007100200025