Micro-PIXE analysis of carbonates and silicates: Tracking fluid flow in crustal environments
Détails
ID Serval
serval:BIB_BD5F58574289
Type
Article: article d'un périodique ou d'un magazine.
Collection
Publications
Institution
Titre
Micro-PIXE analysis of carbonates and silicates: Tracking fluid flow in crustal environments
Périodique
Nuclear Instruments and Methods in Physics Research Section B - Beam Interactions with Materials and Atoms
ISSN-L
0168-583X
Statut éditorial
Publié
Date de publication
1997
Peer-reviewed
Oui
Volume
130
Pages
660-665
Langue
anglais
Résumé
Proton-induced X-ray (PIXE) analyses on a micro-scale of trace-element
(TE) variations in metamorphic and hydrothermal minerals can provide
insights into fluid-flow processes in lithospheric environments. The Los
Alamos nuclear microprobe was used to determine in situ TE abundances in
minerals from the Ubehebe Peak contact aureole and from Apennine
ophicalcites. In these two crustal environments, known to have
experienced significant fluid flow, TE variability in minerals zoning in
grains, analyses of multiple mineral generations in single samples, and
analyses of grains from spatially-resolved hand-samples provides
information on the chemical evolution of fluid-flow systems during
geologic processes. (C) 1997 Elsevier Science B.V.
(TE) variations in metamorphic and hydrothermal minerals can provide
insights into fluid-flow processes in lithospheric environments. The Los
Alamos nuclear microprobe was used to determine in situ TE abundances in
minerals from the Ubehebe Peak contact aureole and from Apennine
ophicalcites. In these two crustal environments, known to have
experienced significant fluid flow, TE variability in minerals zoning in
grains, analyses of multiple mineral generations in single samples, and
analyses of grains from spatially-resolved hand-samples provides
information on the chemical evolution of fluid-flow systems during
geologic processes. (C) 1997 Elsevier Science B.V.
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02/10/2012 20:34
Dernière modification de la notice
20/08/2019 16:31
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