Microfabrics, grain-size-distributions and grain surface textures in Late Pleistocene basin sediments of Brandenburg (Northern Barnim)
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Lutz.Schirrmeister [ at ] awi.de
Abstract
The Biesenthal Basin formed by thawing of dead ice, is located at the northern rim of the Barnim Plateau north of Berlin; in it sedimentary processes varied considerably during the Late Weichsel Glacial Period. The glacifluviolimnic, limnic and aeolian sediments were deposited on the shore of a periglacial water within the area shaped by the last glacial advance; presently it is located at the border between lowlands and plateau. The sedimentary sequence is characterized by variations and deformations at the scale of micrometers. -from Author
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47060
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https://www.doi.org/10.1127/zfgsuppl/99/1995/75
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Schirrmeister, L.
(1995):
Microfabrics, grain-size-distributions and grain surface textures in Late Pleistocene basin sediments of Brandenburg (Northern Barnim)
,
Zeitschrift für Geomorphologie Supplement Volumes,
99
,
pp. 75-89
.
doi: https://www.doi.org/10.1127/zfgsuppl/99/1995/75
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