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  3. Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup?
 

Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup?

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BORIS DOI
10.7892/boris.81398
Publisher DOI
10.1016/j.lithos.2015.09.016
Date of Publication
2015
Publication Type
article
Subject(s)
500 - Science::550 - Earth sciences & geology
Language(s)
en
Contributor(s)
Schmaedicke, E.
Will, T.
Mezger, Klausorcid-logo
Institut für Geologie
Additional Credits
Institut für Geologie
Series
Lithos
Publisher
Elsevier
ISSN
0024-4937
Access(Rights)
restricted
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