Origins of Os-isotope and platinum-group element compositions of metasomatized peridotite and cumulate pyroxenite xenoliths from Kharchinsky Volcano, Kamchatka-Reference-Cited by-同舟云学术

Origins of Os-isotope and platinum-group element compositions of metasomatized peridotite and cumulate pyroxenite xenoliths from Kharchinsky Volcano, Kamchatka

Published:2021-04 Issue: Volume:299 Page:130-150
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Siegrist Max,Yogodzinski Gene M.,Bizimis Michael

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference165 articles.

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3. In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle;Alard;Nature,2005

4. The solubility of ruthenium in sulfide liquid: implications for platiunum group mineral stability and sulfide melt-silicate melt partitioning;Andrews;Chem. Geol.,2002

5. Primary platinum mineralization in the Nizhny Tagil and Kachkanar Ultramafic Complexes, Urals, Russia: A genetic model for PGE concentration in chromite-rich zones;Augé;Econ. Geol.,2005

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1. Ancient melt percolation in forearc mantle pyroxenites: Evidence from highly siderophile elements and Os isotope ratios;Geochimica et Cosmochimica Acta;2024-06

2. New Data on the Rock and Mineral Composition of Kharchinsky and Zarechny Volcanoes, Central Kamchatka Depression: Heterogeneity of the Mantle Source and Peculiarities of Magma Evolution in the Crust;Petrology;2023-06

3. Highly siderophile element fractionation during chondrite melting inferred from olivine-rich primitive achondrites;Geochimica et Cosmochimica Acta;2023-06

4. New Data on the Rock and Mineral Composition of Kharchinsky and Zarechny Volcanoes (Central Kamchatka depression): Heterogeneity of the Mantle Source and Peculiarities of Magma Evolution in Crust;Петрология;2023-05-01

5. Metals in Avachinsky peridotite xenoliths with implications for redox heterogeneity and metal enrichment in the Kamchatka mantle wedge;Lithos;2022-03