Redistribution of magnetite during multi–stage serpentinization: Evidence from the Taishir Massif, Khantaishir ophiolite, western Mongolia
Author:
Affiliation:
1. Graduate School of Environmental Studies, Tohoku University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/116/3/116_201130a/_pdf
Reference16 articles.
1. Bach, W., Paulick, H., Garrido, C.J., Ildefonse, B., et al (2006) Unraveling the sequence of serpentinization reactions: Petrography, mineral chemistry, and petrophysics of serpentinites from MAR 15°N (ODP Leg 209, Site 1274). Geophysical Research Letters, 33. https://doi.org/10.1029/2006GL025681
2. Dandar, O., Okamoto, A., Uno, M., Oyanagi, R., et al (2019) Formation of secondary olivine after orthopyroxene during hydration of mantle wedge: evidence from the Khantaishir Ophiolite, western Mongolia. Contribution to Mineralogy and Petrology, 174. https://doi.org/10.1007/s00410–019–1623–1
3. Evans, B.W. (2008) Control of the products of serpentinization by the Fe2+ Mg−1 exchange potential of olivine and orthopyroxene. Journal of Petrology, 49, 1873–1887.
4. Evans, B.W. (2010) Lizardite versus antigorite serpentinite: Magnetite, hydrogen, and life(?). Geology, 38, 879–882.
5. Frost, R.B. and Beard, J.S. (2007) On silica activity and serpentinization. Journal of Petrology, 48, 1351–1368.
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