Origin of amphibole in recrystallized and porphyroclastic mantle xenoliths from the Rhenish Massif: implications for the nature of mantle metasomatism-Reference-Cited by-同舟云学术

Origin of amphibole in recrystallized and porphyroclastic mantle xenoliths from the Rhenish Massif: implications for the nature of mantle metasomatism

Published:1989-01 Issue:3-4 Volume:91 Page:327-340
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Witt G.,Seck H.A.

Publisher

Elsevier BV

Subject

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

Reference41 articles.

1. Petrology and geochemistry of composite ultramafic xenoliths in alkalic basalts and implications for magmatic processes within the mantle;Irving;Am. J. Sci.,1980

2. An example of consequent mantle metasomatism in peridotite inclusions from Nunivak Island, Alaska;Roden;J. Petrol.,1984

3. Petrography, petrology, and geochemistry of xenoliths from the Geronimo Volcanic Field, Southern Arizona;Kempton,1984

4. Amphibole-rich veins in lherzolite xenoliths, Dish Hill and Deadman Lake, California;Wilshire;Am. J. Sci.,1980

5. The mineralogy, geochemistry and origin of lherzolite inclusions in Victorian basanites;Frey;Geochim. Cosmochim. Acta,1974

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