Can Orthopyroxene be Present in the Source of Toro-Ankole, East African Rift, Kamafugites?

Author:

Gurenko Andrey A123,Sobolev Alexander V234

Affiliation:

1. Centre de Recherches Pétrographiques et Géochimiques, UMR 7358, Université de Lorraine, Vandoeuvre-lès-Nancy, France

2. Max-Planck-Institut für Chemie, Mainz, Germany

3. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, Russia

4. Institut des Sciences de la Terre (ISTerre), UMR 5275, Université de Grenoble Alpes, Grenoble, France

Funder

The Wolfgang Paul Award

Alexander von Humboldt Foundation

Russian Academy of Sciences

Max Planck Society

INSU-CNRS

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference134 articles.

1. Internally consistent solution models for Fe–Mg–Mn–Ti oxides;Andersen;American Mineralogist,1988

2. QUILF: a PASCAL program to assess equilibria among Fe–Mg–Ti oxides, pyroxenes, olivine and quartz;Andersen;Computers and Geosciences,1993

3. Petrology of kamafugites and kimberlites from the Alto Paranaíba Alkaline Province, Minas Gerais, Brazil;Araujo;Contributions to Mineralogy and Petrology,2001

4. High pressure experimental studies on a katungite and their bearing on the genesis of some potassium-rich magmas of the West Branch of the African rift;Arima;Journal of Petrology,1983

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