Temporal, isotopic and spatial relations of early paleozoic gondwana-margin arc magmatism, Central Transantarctic Mountains, Antarctica

The Cambrian-Ordovician Ross Orogeny in Antarctica produced a voluminous magmatic belt composed mainly of post-orogenic granitoids. This magmatic belt has strong calc-alkaline characteristics reflecting a convergent-margin origin associated with subduction of paleo-Pacific oceanic lithosphere beneat...

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Bibliographic Details
Main Authors: Goodge, John W, Fanning, Christopher, Norman, Marc, Bennett, Victoria
Format: Article in Journal/Newspaper
Language:unknown
Published: Oxford University Press 2015
Subjects:
Online Access:http://hdl.handle.net/1885/67004