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

Schmädicke E, Will TM, Mezger K (2015)

Publication Status: Published

Publication Type: Journal article, Original article

Publication year: 2015

Journal

Lithos Elsevier

Publisher: Elsevier

Book Volume: 238

Pages Range: 185-206

DOI: 10.1016/j.lithos.2015.09.016

Authors with CRIS profile

Esther Schmädicke Professur für Mineralogie

Involved external institutions

Julius-Maximilians-Universität Würzburg DE Germany (DE) Universität Bern CH Switzerland (CH)

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://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.

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