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The x-ray identification and crystal structures of clay minerals
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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.read more
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Book ChapterDOI
Kolsuz-Ulukisla-Nigde Clays, Central Anatolian Region - Turkey and Petroleum Exploration
TL;DR: Clays are naturally occurring, fine-grained minerals under surface conditions mostly as alteration products with distinct crystal structures as mentioned in this paper and they may show plastic behavior when mixed with sufficient water and become stiff when dried or cooked.
Methodological proposal for rammed-earth wall characterization: Understanding of material in preliminary studies.
Francisco Javier Alejandre Sánchez,J. J. Martín-del-Río,Francisco-Javier Blasco-López,Vicente Flores Alés +3 more
TL;DR: In this article, the authors present a series of analyses and tests to be carried out in historical studies for wall characterization, which can be classified into five groups based on wall properties: chemical and mineralogical composition, physical and hydric properties, mechanical properties, granulometry, and dating.
Clay Mineralogy and Origin of the Huntingdon Fire Clays on Canadian Sumas Mountain, South British Columbia
TL;DR: In this article, the Eocene fire clay seams are separated from each other and overlain by coal partings in Canadian Sumas Mountain, southwest British Columbia, and they are shown to be composed of small domains of fine-grained, interlocking kaolinite flakes in face-to-face contact.
Journal ArticleDOI
Crystal chemical analysis of natural clay material of different genesis
TL;DR: In this article, the results reveal differences both in the composition, structure, properties, morphology and IR spectroscopic characteristics of nontronites of different origin of natural clay material.
Journal ArticleDOI
Low-frequency dielectric relaxation of Cs+-ions in single-crystals of mica-type layer-silicates
TL;DR: In this article, ausammenfassung Messungen der dielektrischen Permeabilitat ϵ' und des dielektriche Absorptionskoeffizienten ϵ″ an Einkristallen von glimmerartigen Schichtsilicaten (Vermiculiten) im Frequenzbereich zwischen 30 Hz and 10 MHz zeigen ein niederfrequentes diele-ktrisches Absorbgebiet.