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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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Sedimentology, Mineral Facies, and Petrofabric of the Meaford–Dundas Formation (Upper Ordovician) in Southern Ontario

TL;DR: The Meaford-Dundas Formation in southern Ontario is a medium gray shale with good fissility and resistant interbeds of gray fossiliferous limestones and siltstones as mentioned in this paper.
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Clay mineralogy at Rothamsted; 1934-1988

TL;DR: Soil clay mineralogy at Rothamsted began in the early 1930s, and quickly focused on technique, swelling minerals, micas and sorption phenomena as discussed by the authors, which continued for the next 40 years.
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Fragipan soils of Condroz (Belgium): Mineralogical, chemical and physical aspects in relation with their genesis

J.M. Lozet, +1 more
- 01 Jun 1971 - 
TL;DR: In this paper, the authors report the results of mineralogical and chemical investigations undertaken in view of characterizing their fraginan horizons, and suggest that such irreversible and important modifications affecting the fragipan zone could be the result of periglacial processes implicated in the so called "fragipan catastrophic development".
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Glauconite from Paleogene volcano-terrigenous rocks in Western Kamchatka

TL;DR: In this paper, it was shown that glauconite-bearing interbeds are widespread in layer-by-layer studied sections on the Sea of Okhotsk coast (Mainach section) and Kheisliveem River valley (Kavran section), the volcanoterrigenous rocks of the Kovachin, Amanin, and Gakkhin formations of the Paleogene in western Kamchatka (Upper Eocene-Lower Oligocene boundary beds).