Isotopic fractionation during congruent dissolution, precipitation and at equilibrium: Evidence from Mg isotopes
This study provides direct experimental evidence of magnesium (Mg) isotope fractionation between an aqueous fluid and magnesite during its congruent dissolution, precipitation and at equilibrium. Closed-system batch reactor experiments were performed at temperatures from 120 to 200 °C and at 15 or 3...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
2012-09-01.
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Subjects: | |
Online Access: | Get fulltext |