Fossil subduction zone origin for magmas in the Ferrar Large Igneous Province, Antarctica: Evidence from PGE and Os isotope systematics in the Basement Sill of the McMurdo Dry Valleys-Reference-Cited by-同舟云学术

Fossil subduction zone origin for magmas in the Ferrar Large Igneous Province, Antarctica: Evidence from PGE and Os isotope systematics in the Basement Sill of the McMurdo Dry Valleys

Published:2019-01 Issue: Volume:506 Page:507-519
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Choi Sung Hi,Mukasa Samuel B.,Ravizza Greg,Fleming Thomas H.,Marsh Bruce D.,Bédard Jean H.J.

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference101 articles.

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3. Large igneous provinces, delamination, and fertile mantle;Anderson;Elements,2005

4. Enriched mantle – Dupal signature in the genesis of the Jurassic Ferrar tholeiites from Prince Albert Mountains (Victoria Land, Antarctica);Antonini;Contrib. Mineral. Petrol.,1999

5. Fractionation of the noble metals by physical processes;Ballhaus;Contrib. Mineral. Petrol.,2006

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