Evidence from Antarctic mantle peridotite xenoliths for changes in mineralogy, geochemistry and geothermal gradients beneath a developing rift-Reference-Cited by-同舟云学术

Evidence from Antarctic mantle peridotite xenoliths for changes in mineralogy, geochemistry and geothermal gradients beneath a developing rift

Published:2006-06 Issue:12 Volume:70 Page:3096-3120
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Foley S.F.,Andronikov A.V.,Jacob D.E.,Melzer S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference106 articles.

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4. Varying glass compositions in deep-seated inclusions from alkaline–ultramafic rocks of Jetty Peninsula (East Antarctica): evidence for mantle metasomatism;Andronikov,1997

5. Implication of Sm–Nd isotopic systematics to the events recorded in the mantle-derived xenoliths from the Jetty Peninsula, East Antarctica;Andronikov;Terra Antarct.,1995

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