Os-isotope variability within sulfides from podiform chromitites-Reference-Cited by-同舟云学术

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Os-isotope variability within sulfides from podiform chromitites

Published:2012-01 Issue: Volume:291 Page:224-235
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

González-Jiménez José M.,Gervilla Fernando,Griffin William L.,Proenza Joaquín A.,Augé Thierry,O'Reilly Suzanne Y.,Pearson Norman J.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference86 articles.

1. Osmium isotope systematics of the Proterozoic and Phanerozoic ophiolitic chromitites: in situ ion probe analysis of primary Os-rich PGM;Ahmed;Earth and Planetary Science Letters,2006

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

3. The solubility of ruthenium in sulfide liquid : implications for platinum group mineral stability and sulfide metal-silicate melt partitioning;Andrews;Chemical Geology,2002

4. Podiform chromitites of the Tari-Misaka Ultramafic Complex, Southwestern Japan, as mantle-melt interaction products;Arai;Economic Geology,1994

5. Mantle formation and evolution, Slave Craton: constraints from HSE abundances and Re–Os isotope systematics of sulfide inclusions in mantle xenocrysts;Aulbach;Chemical Geology,2004

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4. A record of metasomatism and crustal contamination of the Mediterranean lithosphere in chromitites of the Orhaneli Ophiolite Complex (NW Türkiye);Journal of Asian Earth Sciences;2022-09

5. Origin and depositional history of platinum-group minerals in placers – A critical review of facts and fiction;Ore Geology Reviews;2022-05

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