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

Schmaedicke, E.; Will, T.; Mezger, Klaus (2015). Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup? Lithos, 238, pp. 185-206. Elsevier 10.1016/j.lithos.2015.09.016

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Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Institute of Geological Sciences

UniBE Contributor:

Mezger, Klaus

Subjects:

500 Science > 550 Earth sciences & geology

ISSN:

0024-4937

Publisher:

Elsevier

Language:

English

Submitter:

Klaus Mezger

Date Deposited:

20 Jun 2016 17:15

Last Modified:

20 Jun 2016 17:15

Publisher DOI:

10.1016/j.lithos.2015.09.016

BORIS DOI:

10.7892/boris.81398

URI:

https://boris.unibe.ch/id/eprint/81398

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