New age constraints for Grenville-age metamorphism in western central Dronning Maud Land (East Antarctica), and implications for the palaeogeography of Kalahari in Rodinia
New SHRIMP zircon data from Gjelsvikfjella and Mühlig-Hofmann-Gebirge (East Antarctica) indicate that the metamorphic basement is composed of Grenville-age rocks that are most likely part of the north-eastern continuation of the Namaqua-Natal-Maud Belt.
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Springer
2015
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/86041 |
Summary: | New SHRIMP zircon data from Gjelsvikfjella and Mühlig-Hofmann-Gebirge (East Antarctica) indicate that the metamorphic basement is composed of Grenville-age rocks that are most likely part of the north-eastern continuation of the Namaqua-Natal-Maud Belt. |
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