Structure of the Deep Freeze Range–Eisenhower Range of the Wilson Terrane (North Victoria Land, Antarctica): emplacement of magmatic intrusions in the Early Palaeozoic deformed margin of the East Antarctic Craton

In North Victoria Land (Antarctica), the Wilson Terrane is a portion of the palaeomargin of the East Antarctic Craton, deformed during the Late Cambrian–Early Ordovician Ross Orogeny. Crustal deformation, from westward subduction of the palaeo Pacific plate and terrane accretion on this palaeomargin...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Musumeci, Giovanni, Pertusati, Piero
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2000
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102000000122
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102000000122