DOI: 10.1016/j.quascirev.2015.05.033
Scopus记录号: 2-s2.0-84935020619
论文题名: Development of the topography-controlled Upper Odra ice lobe (Scandinavian Ice Sheet) in the fore-mountain area of southern Poland during the Saalian glaciation
作者: Salamon T.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2015
卷: 123 起始页码: 1
结束页码: 15
语种: 英语
英文关键词: Pleistocene ice-sheet dynamics
; S Poland
; Topography-controlled ice lobe
Scopus关键词: Glacial geology
; Glaciers
; Landforms
; Lithology
; Topography
; Ice flow dynamics
; Ice sheet dynamics
; Low permeability
; Mountain ranges
; Pore-water pressures
; Primary factors
; Quaternary deposits
; S Poland
; Ice
; basal ice
; ice flow
; lithology
; lowland environment
; Neogene
; porewater
; Saalian
; Scandinavian Ice Sheet
; Silesian
; subglacial environment
; till
; topography
; Poland
英文摘要: During the Saalian (Drenthe) glaciation, the Upper Odra ice lobe constituted the most southern part of the Scandinavian Ice Sheet in central Europe. The lobe was situated in an area with varied topography in the foreland of a mountain range. The ice lobe had a complex form because it was subdivided into several smaller sublobes. The primary factors that controlled the lobe were investigated. It was found that the ice-lobe development depended largely on the topography, but the lithology of the ice sheet substratum was also highly important. The topography controlled the main movement direction of the ice and caused a concentration of the ice flow in the axial part of the Silesian Lowland between subglacial morphological barriers, which thereby formed a corridor of relatively fast flowing ice, which was probably streaming and which supplied the lobe. The topography also determined the ice flow within the lobe, which strongly matched the valley system. The presence of sediments with relatively low permeability at the base of the lobe (the Quaternary deposits are underlain by Neogene clays) caused high pore-water pressure in the subglacial zone and triggered the basal movement of the ice sheet, which promoted a rapid flow of the ice and favoured the development of the lobe. The basal tills deposited from the active and passive ice and extant till patches without a fluvioglacial cover atop some parts of the studied area indicate spatially varying ice flow dynamics, especially in the later stage of glaciation. Certain parts of the lobe underwent stagnation, while in other parts, the ice was probably still active. The varied behaviour of the ice within the lobe was determined primarily by the topography and lithology of the substratum, which produced spatially varied marginal compression and basal friction. A model of the development of the lobe is proposed. © 2015 Elsevier Ltd. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59872
Appears in Collections: 过去全球变化的重建
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作者单位: Faculty of Earth Science, University of Silesia, Bȩdzińska 60, Sosnowiec, Poland
Recommended Citation:
Salamon T.. Development of the topography-controlled Upper Odra ice lobe (Scandinavian Ice Sheet) in the fore-mountain area of southern Poland during the Saalian glaciation[J]. Quaternary Science Reviews,2015-01-01,123