Platinum-bearing chromite layers are caused by pressure reduction during magma ascent

Some basaltic melts become first superheated upon their ascent towards the Earth’s surface and then saturated in chromite alone after cooling in shallow chambers. Here the authors show that large volumes of these chromite-only-saturated melts are responsible for monomineralic layers of massive chrom...

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Autores principales: Rais Latypov, Gelu Costin, Sofya Chistyakova, Emma J. Hunt, Ria Mukherjee, Tony Naldrett
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/134b7f8f95414949a93b6a391e02672f
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spelling oai:doaj.org-article:134b7f8f95414949a93b6a391e02672f2021-12-02T14:40:55ZPlatinum-bearing chromite layers are caused by pressure reduction during magma ascent10.1038/s41467-017-02773-w2041-1723https://doaj.org/article/134b7f8f95414949a93b6a391e02672f2018-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-02773-whttps://doaj.org/toc/2041-1723Some basaltic melts become first superheated upon their ascent towards the Earth’s surface and then saturated in chromite alone after cooling in shallow chambers. Here the authors show that large volumes of these chromite-only-saturated melts are responsible for monomineralic layers of massive chromitites in layered intrusions.Rais LatypovGelu CostinSofya ChistyakovaEmma J. HuntRia MukherjeeTony NaldrettNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-7 (2018)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Rais Latypov
Gelu Costin
Sofya Chistyakova
Emma J. Hunt
Ria Mukherjee
Tony Naldrett
Platinum-bearing chromite layers are caused by pressure reduction during magma ascent
description Some basaltic melts become first superheated upon their ascent towards the Earth’s surface and then saturated in chromite alone after cooling in shallow chambers. Here the authors show that large volumes of these chromite-only-saturated melts are responsible for monomineralic layers of massive chromitites in layered intrusions.
format article
author Rais Latypov
Gelu Costin
Sofya Chistyakova
Emma J. Hunt
Ria Mukherjee
Tony Naldrett
author_facet Rais Latypov
Gelu Costin
Sofya Chistyakova
Emma J. Hunt
Ria Mukherjee
Tony Naldrett
author_sort Rais Latypov
title Platinum-bearing chromite layers are caused by pressure reduction during magma ascent
title_short Platinum-bearing chromite layers are caused by pressure reduction during magma ascent
title_full Platinum-bearing chromite layers are caused by pressure reduction during magma ascent
title_fullStr Platinum-bearing chromite layers are caused by pressure reduction during magma ascent
title_full_unstemmed Platinum-bearing chromite layers are caused by pressure reduction during magma ascent
title_sort platinum-bearing chromite layers are caused by pressure reduction during magma ascent
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/134b7f8f95414949a93b6a391e02672f
work_keys_str_mv AT raislatypov platinumbearingchromitelayersarecausedbypressurereductionduringmagmaascent
AT gelucostin platinumbearingchromitelayersarecausedbypressurereductionduringmagmaascent
AT sofyachistyakova platinumbearingchromitelayersarecausedbypressurereductionduringmagmaascent
AT emmajhunt platinumbearingchromitelayersarecausedbypressurereductionduringmagmaascent
AT riamukherjee platinumbearingchromitelayersarecausedbypressurereductionduringmagmaascent
AT tonynaldrett platinumbearingchromitelayersarecausedbypressurereductionduringmagmaascent
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