Characterization of Iron-Rich Phyllosilicates Formed at Different Fe/Si Ratios
Author:
Publisher
Springer Science and Business Media LLC
Subject
Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Soil Science,Water Science and Technology
Link
https://link.springer.com/content/pdf/10.1007/s42860-022-00204-6.pdf
Reference68 articles.
1. Badaut, D., Besson, G., Decarreau, A., & Rautureau, R. (1985). Occurrence of a ferrous, trioctahedral smectite in recent sediments of Atlantis II Deep, Red Sea. Clay Minerals, 20(3), 389–404. https://doi.org/10.1180/claymin.1985.020.3.09
2. Badaut, D., Decarreau, A., & Besson, G. (1992). Ferripyrophyllite and related Fe3+-rich 2:1 clays in recent deposits of Atlantis II Deep, Red Sea. Clay Minerals, 27(2), 227–244. https://doi.org/10.1180/claymin.1992.027.2.07
3. Bailey, S. W. (1988). In S. W. Bailey (Ed.), Volume 19: Hydrous Phyllosilicates (Exclusive of Micas). Mineralogical Society of America.
4. Baker, L. L., & Strawn, D. G. (2014). Temperature effects on the crystallinity of synthetic nontronite and implications for nontronite formation in Columbia river basalts. Clays and Clay Minerals, 62(2), 89–101. https://doi.org/10.1346/CCMN.2014.0620202
5. Baldermann, A., Warr, L. N., Letofsky-Papst, I., & Mavromatis, V. (2015). Substantial iron sequestration during green-clay authigenesis in modern deep-sea sediments. Nature Geoscience, 811, 885–889. https://doi.org/10.1038/ngeo2542
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