Highly siderophile element geochemistry of peridotites and pyroxenites from Horní Bory, Bohemian Massif: Implications for HSE behaviour in subduction-related upper mantle-Reference-Cited by-同舟云学术

Highly siderophile element geochemistry of peridotites and pyroxenites from Horní Bory, Bohemian Massif: Implications for HSE behaviour in subduction-related upper mantle

Published:2013-01 Issue: Volume:100 Page:158-175
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Ackerman Lukáš,Pitcher Lynnette,Strnad Ladislav,Puchtel Igor S.,Jelínek Emil,Walker Richard J.,Rohovec Jan

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference92 articles.

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3. Determination of total sulfur in fifteen geological materials using Inductively Coupled Plasma-Optical Emission Spectrometry (ICP-OES) and Combustion/Infrared spectrometry;Ackerman;Geostand. Geoanal. Res,2012

4. Nonchondritic distribution of the highly siderophile elements in mantle sulphides;Alard;Nature,2000

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

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