Reduced amphibolite facies conditions in the Precambrian continental crust of the Siberian craton recorded by mafic granulite xenoliths from the Udachnaya kimberlite pipe, Yakutia

Author:

Perchuk A.L.,Sapegina A.V.,Safonov O.G.,Yapaskurt V.O.,Shatsky V.S.,Malkovets V.G.

Funder

Russian Academy of Sciences

Russian Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference106 articles.

1. Metasomatism in lithospheric mantle roots: constraints from whole-rock and mineral chemical composition of deformed peridotite xenoliths from kimberlite pipe Udachnaya;Agashev;Lithos,2013

2. A revision of the garnet-clinopyroxene Fe 2+-Mg exchange geothermometer;Ai;Contrib. Miner. Petrol.,1994

3. Model for the Ti magnetite or ilmenite geothermometers and oxygen barometers;Anderson;Trans. Geophysical Union,1985

4. Phenocrysts and glass inclusions and their bearing on oxidation and mixing of basaltic magmas, Kilauea volcano, Hawaii;Anderson;Am. Mineral.,1972

5. Precambrian tectonic environments;Anhaeusser;Annu. Rev. Earth Planet. Sci.,1975

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