Morphoscopy and Morphometry of Quartz Grains from Loess and Buried Soil Layers

A complex method is suggested for the study of surfaces of sand grains. With this method, middle-and late Pleistocene loess-palaeosol sequences of the Russian Plain, Dnieper Basin, were studied. Surface texture of grains pointed to a dry and cold climate for their formation. During deposition of loe...

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Veröffentlicht in:GeoJournal 1995-06, Vol.36 (2/3), p.143-149
Hauptverfasser: Velichko, Andrej A., Timireva, Svetlana N.
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description A complex method is suggested for the study of surfaces of sand grains. With this method, middle-and late Pleistocene loess-palaeosol sequences of the Russian Plain, Dnieper Basin, were studied. Surface texture of grains pointed to a dry and cold climate for their formation. During deposition of loess layers predominantly aeolian and cryogenic processes formed the grain surfaces. During interglacial and interstadial periods chemical weathering dominated.
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subjects Forest soils
Granulometrical and Morphoscopical Methods
Loess
Loess soils
Paleoecology
Paleogeography
Quartz
Russia
Sand
Sedimentary soils
Sediments
Soil chemistry
Soil horizons
Soils
Surface texture
title Morphoscopy and Morphometry of Quartz Grains from Loess and Buried Soil Layers
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