Hydration behavior by X-ray diffraction profile fitting of smectite-bearing minerals in a Plio-Pleistocene mudrock from Eugene Island, Gulf of Mexico

Clay mineral hydration and dehydration processes are reversible at temperatures

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Bibliographic Details
Published in:Marine and petroleum geology 2019-04, Vol.102, p.86-100
Main Authors: Day-Stirrat, Ruarri J., Bryndzia, L. Taras, Schleicher, Anja M., Adriaens, Rieko, Hofmann, Ronny, Flemings, Peter B.
Format: Article
Language:English
Subjects:
Clay minerals
Dehydration
Hydration
Mixed-layer clays
Overpressure
Pore pressure
Relative humidity
Smectite
Water activity
X-ray profile modelling
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Description
Summary:Clay mineral hydration and dehydration processes are reversible at temperatures
ISSN:0264-8172
DOI:10.1016/j.marpetgeo.2018.12.008