Variation of Mg isotopes during mineral dissolution at pH = 1 and T = 25 °C: Part 2. Olivine and pyroxene

Abstract Background The high reactivity of mafic minerals, such as olivine and pyroxene, plays a crucial role in controlling the global magnesium (Mg) flux and its isotopic composition. This study investigates the mechanisms and extent of Mg isotope fractionation during the dissolution of these mine...

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Bibliographic Details
Main Author: Jong-Sik Ryu
Format: Article
Language:English
Published: SpringerOpen 2025-02-01
Series:Journal of Analytical Science and Technology
Subjects:
Online Access:https://doi.org/10.1186/s40543-025-00479-z
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