Crossref journal-article
Mineralogical Society
Clay Minerals (7149)
Abstract

AbstractA trioctahedral, ferrous smectite has been located in the uppermost deposits of Atlantis II Deep, SW basin, Red Sea. This clay is very unstable when removed from its environment of formation and, for example, oxidizes during desiccation under laboratory conditions. Only X-ray transmission diffraction study of the mud itself demonstrates the trioctahedral character of the clay. Electron-optical investigation shows that oxidation within the octahedral sheet creates a juxtaposition of dioctahedral and trioctahedral sub-lattices in the same particle. Ferrous smectite authigenesis is located near the hydrothermal spring outlets of the Atlantis II Deep.

Bibliography

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.

Authors 4
  1. D. Badaut (first)
  2. G. Besson (additional)
  3. A. Decarreau (additional)
  4. R. Rautureau (additional)
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Dates
Type When
Created 18 years, 8 months ago (Dec. 8, 2006, 11:50 p.m.)
Deposited 1 year, 6 months ago (Feb. 8, 2024, 4:28 p.m.)
Indexed 1 year, 1 month ago (July 21, 2024, 6:30 a.m.)
Issued 40 years ago (Sept. 1, 1985)
Published 40 years ago (Sept. 1, 1985)
Published Online 7 years, 1 month ago (July 9, 2018)
Published Print 40 years ago (Sept. 1, 1985)
Funders 0

None

@article{Badaut_1985, title={Occurrence of a ferrous, trioctahedral smectite in Recent sediments of Atlantis II Deep, Red Sea}, volume={20}, ISSN={1471-8030}, url={http://dx.doi.org/10.1180/claymin.1985.020.3.09}, DOI={10.1180/claymin.1985.020.3.09}, number={3}, journal={Clay Minerals}, publisher={Mineralogical Society}, author={Badaut, D. and Besson, G. and Decarreau, A. and Rautureau, R.}, year={1985}, month=sep, pages={389–404} }