Late Neoproterozoic/Early Palaeozoic events in central Dronning Maud Land and significance for the southern extension of the East African Orogen into East Antarctica
New SHRIMP zircon data from Gjelsvikfjella and Mühlig-Hofmann-Gebirge indicate that the metamorphic basement is composed of Grenville-age rocks that are most likely part of the northeastern continuation of the Namaqua-Natal-Maud Belt. High-grade overprin
Published in: | Precambrian Research |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/86047 https://doi.org/10.1016/S0301-9268(03)00125-6 https://openresearch-repository.anu.edu.au/bitstream/1885/86047/5/MigratedxPub14785_2003.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/86047/7/01_Jacobs_Late_Neoproterozoic%2FEarly_2003.pdf.jpg |
Summary: | New SHRIMP zircon data from Gjelsvikfjella and Mühlig-Hofmann-Gebirge indicate that the metamorphic basement is composed of Grenville-age rocks that are most likely part of the northeastern continuation of the Namaqua-Natal-Maud Belt. High-grade overprin |
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