Increased mantle heat flow with on-going rifting of the West Antarctic rift system inferred from characterisation of plagioclase peridotite in the shallow Antarctic mantle-Reference-Cited by-同舟云学术

Increased mantle heat flow with on-going rifting of the West Antarctic rift system inferred from characterisation of plagioclase peridotite in the shallow Antarctic mantle

Published:2014-03 Issue: Volume:190-191 Page:173-190
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Martin A.P.,Cooper A.F.,Price R.C.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference137 articles.

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