Magmatic belts in accretionary margins, a key for tectonic evolution: the Tonalite Belt of North Victoria Land (East Antarctica)

Occurring in the Early Palaeozoic palaeomargin of the East Antarctica Craton, the Tonalite Belt of North Victoria Land is a narrow linear magmatic belt up to 200 km long, made up of strongly foliated tonalitic and granodioritic intrusions. They were synkinematically emplaced into the Lanterman-Murch...

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Bibliographic Details
Published in:Journal of the Geological Society
Main Author: MUSUMECI, GIOVANNI
Other Authors: Musumeci, Giovanni
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
Online Access:http://hdl.handle.net/11568/161306
https://doi.org/10.1144/gsjgs.156.1.0177