Fe (super 3+) distribution in oxidized olivine; a synchrotron micro-XANES study-Reference-Cited by-同舟云学术

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Fe (super 3+) distribution in oxidized olivine; a synchrotron micro-XANES study

Published:1998-12-01 Issue:11-12 Part 1 Volume:83 Page:1361-1365
ISSN:0003-004X
Container-title:American Mineralogist
language:en
Short-container-title:American Mineralogist

Author:

Dyar M.,Delaney Jeremy S.,Sutton Stephen R.,Schaffer Martha W.

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology,Geophysics

Cited by 52 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Arc magmatic evolution and porphyry copper deposit formation under compressional regime: A geochemical perspective from the Toquepala arc in Southern Peru;Earth-Science Reviews;2023-05

2. Iron redox analysis of silicate-based minerals and glasses using synchrotron X-ray absorption and laboratory X-ray emission spectroscopy;Journal of Non-Crystalline Solids;2022-02

3. Silicate minerals as a direct source of limiting nutrients: Siderophore synthesis and uptake promote ferric iron bioavailability from olivine and microbial growth;Geobiology;2021-06-09

4. Are the thermodynamic properties of natural and synthetic Mg2SiO4-Fe2SiO4 olivines the same?;American Mineralogist;2021-02-01

5. Geochemical and mineralogical changes in magnetite Fe-ore tailings induced by biomass organic matter amendment;Science of The Total Environment;2020-07

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