Iron isotope and trace metal variations during mantle metasomatism: In situ study on sulfide minerals from peridotite xenoliths from Nógrád-Gömör Volcanic Field (Northern Pannonian Basin)-Reference-Cited by-同舟云学术

Iron isotope and trace metal variations during mantle metasomatism: In situ study on sulfide minerals from peridotite xenoliths from Nógrád-Gömör Volcanic Field (Northern Pannonian Basin)

Published:2021-09 Issue: Volume:396-397 Page:106238
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Patkó Levente,Ciazela Jakub,Aradi László Előd,Liptai Nóra,Pieterek Bartosz,Berkesi Márta,Lazarov Marina,Kovács István János,Holtz François,Szabó Csaba

Funder

Hungarian Academy of Sciences

Hungarian Government

Polish Academy of Sciences

European Commission

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference82 articles.

1. Non-chondritic distribution of the highly siderophile elements in mantle sulphides;Alard;Nature,2000

2. Volatile-rich metasomatism in Montferrier xenoliths (Southern France): Implications for the abundances of chalcophile and highly siderophile elements in the subcontinental mantle;Alard;J. Petrol.,2011