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Journal Article

Particle size distribution of saliferous clays in the German Zechstein

Sediments and environmental geochemistry: selected aspects and case histories (1990) 197-209
DOI: 10.1007/978-3-642-75097-7_11
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Abstract

The striking correspondence between grain size distribution of red clays of the Rotliegend and loess supports Sonnenfeld's hypothesis, in which a geological relationship between evaporite periods during geological history and their immediately preceding glaciations, is suggested. -from Author

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Kuhn, R. (1990). Particle size distribution of saliferous clays in the German Zechstein. Sediments and Environmental Geochemistry: Selected Aspects and Case Histories, 197–209. https://doi.org/10.1007/978-3-642-75097-7_11

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