Trace element catalyses mineral replacement reactions and facilitates ore formation.
Journal
Nature communications
ISSN: 2041-1723
Titre abrégé: Nat Commun
Pays: England
ID NLM: 101528555
Informations de publication
Date de publication:
02 Mar 2021
02 Mar 2021
Historique:
received:
03
09
2020
accepted:
19
01
2021
entrez:
3
3
2021
pubmed:
4
3
2021
medline:
4
3
2021
Statut:
epublish
Résumé
Reaction-induced porosity is a key factor enabling protracted fluid-rock interactions in the Earth's crust, promoting large-scale mineralogical changes during diagenesis, metamorphism, and ore formation. Here, we show experimentally that the presence of trace amounts of dissolved cerium increases the porosity of hematite (Fe
Identifiants
pubmed: 33654089
doi: 10.1038/s41467-021-21684-5
pii: 10.1038/s41467-021-21684-5
pmc: PMC7925538
doi:
Types de publication
Journal Article
Langues
eng
Sous-ensembles de citation
IM
Pagination
1388Subventions
Organisme : Society of Economic Geologists Foundation (SEG Foundation)
ID : SRG_17-31
Références
Science. 2014 Mar 28;343(6178):1441-2
pubmed: 24675943