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The x-ray identification and crystal structures of clay minerals

George Brown
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The article was published on 1961-01-01 and is currently open access. It has received 966 citations till now. The article focuses on the topics: Clay minerals.

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Journal ArticleDOI

Disordered structural states in the dehydration of goethite and diaspore.

TL;DR: In this paper, satellite reflections occur close to the hematite diffraction spots and disappear on further heating, which correspond to a sinusoidal or square-wave structure amplitude modulation along the c-axis of the Hematite and corundum crystallites.
Journal ArticleDOI

Clay Mineralogy of Kope and Fairview Formations (Cincinnatian) in the Cincinnati Area

TL;DR: In this article, a detailed study of the clay mineralogy of portions of the Kope and Fairview (Cincinnatian) formations of Cincinnati, Ohio reveals a suite composed of illite, chlorite, vermiculite, and some mixed illite-montmorillonite.
Journal ArticleDOI

Depositional and diagenetic signatures of Late Eocene–Oligocene sediments, South Carolina

TL;DR: In this paper, Binocular microscopic examination, scanning electron microscopic/energy dispersive X-ray (SEM/EDX) observations, and Xray diffraction (XRD) analyses indicate that onshore Late Eocene to Late Oligocene Barnwell Group sediments are transitional facies ranging from high-energy fluvial deposits to offshore siliciclastic shelf sands.
Journal ArticleDOI

Correlation of variations in trace elements and mineralogy of the Esopus Formation, Kingston, New York

TL;DR: In this article, X-ray diffraction data and spectrographic analyses are used to strengthen the meaning of this subdivision and to define the Esopus Fm. and separate it from enclosing stratigraphic units.
Book ChapterDOI

Cenozoic Clay Mineralogy of Sites 604 and 605, New Jersey Transect, Deep Sea Drilling Project Leg 93

TL;DR: Hinte et al. as mentioned in this paper examined the clay mineralogy of Cenozoic sediment samples from Deep Sea Drilling Project Sites 604 and 605 on the upper continental rise off New Jersey indicates that sediment deposition of two different clay mineral facies has occurred.