Trace Element Partitioning Dualism under Mineral–Fluid Interaction: Origin and Geochemical Significance

Trace Element Partitioning Dualism under Mineral–Fluid Interaction: Origin and Geochemical Significance

Trace element (TE) partitioning in the system “mineral-hydrothermal solution” is studied by the method of thermo-gradient crystal growth coupled with internal sampling of a fluid phase. The analytical procedure used enables evaluating of structurally bound and superficially bound...

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Bibliographic Details
Main Authors: Vladimir L. Tauson, Sergey V. Lipko, Nikolay V. Smagunov, Raisa G. Kravtsova
Format: Article
Language:English
Published: MDPI AG 2018-06-01
Series:Minerals
Subjects:
trace elements
partitioning
precious metals
rare earth elements
hydrothermal experiment
partition and co-crystallization coefficients
structurally and superficially bound modes
pyrite
magnetite
hematite
single crystals
AAS-GF
ICP-MS
XPS
Online Access:http://www.mdpi.com/2075-163X/8/7/282

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http://www.mdpi.com/2075-163X/8/7/282

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