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

Journal article
(Original article)


Publication Details

Author(s): Schmädicke E, Will TM, Mezger K
Journal: Lithos
Publisher: Elsevier
Publication year: 2015
Volume: 238
Pages range: 185-206
ISSN: 0024-4937


FAU Authors / FAU Editors

Schmädicke, Esther Prof. Dr.
Professur für Mineralogie


External institutions with authors

Julius-Maximilians-Universität Würzburg
Universität Bern


How to cite

APA:
Schmädicke, E., Will, T.M., & Mezger, K. (2015). Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup? Lithos, 238, 185-206. https://dx.doi.org/10.1016/j.lithos.2015.09.016

MLA:
Schmädicke, Esther, Thomas M. Will, and Klaus Mezger. "Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup?" Lithos 238 (2015): 185-206.

BibTeX: 

Last updated on 2019-21-01 at 09:23

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