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STOP 5: Veselava end moraine, north-western Vidzeme Upland [PDF]

open access: yes, 2014
Krievāns, Māris   +2 more
core   +1 more source

Relationships between the macroscale sedimentology and micromorphology of glacigenic diamictons in south-central British Columbia

open access: yes, 2008
This research explores relationships between the macroscale sedimentology and micromorphology of glacigenic diamictons associated with the last Cordilleran Ice Sheet in south-central B.C., and tests the hypothesis that diamictons classified using traditional definitions and sedimentological criteria have unique micromorphologies.
openaire   +1 more source
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Sedimentology and depositional environments of the Lund Diamicton, southern Sweden

Boreas, 1990
The Lund Diamicton (earlier named Lund Till) in SW Skåne, S. Sweden, is a glacioaquatic sediment consisting of clay and massive and laminated diamictons. It is characterized by clasts derived from the Baltic depression and its depositional history can be summarized as follows: After deglaciation, large fields of stagnant ice remained in the area and a ...
KÄRSTIN MALMBERG PERSSON   +1 more
exaly   +2 more sources

A weathered diamicton beneath Upper Weichselian sediments at Silvereke, southeastern Sweden

Gff, 1996
Abstract An at least 2 m thick, weathered, non‐glacial diamicton, buried beneath a 6 m thick Upper Weichselian glaciogenic sequence at Silvereke in SE Sweden, is composed of variously coloured angular/rhombohedral to rounded clasts set in a red or reddish‐brown matrix of clayey silty sand.
Mats Olvmo   +3 more
exaly   +2 more sources

Problems associated with seismic facies analysis of diamicton-dominated, shelf glacigenic sequences

Geo-Marine Letters, 1990
Diamicton-dominated shelf glacigenic sequences are characterized on high-resolution seismic records by a structureless to chaotic acoustic texture, often with abundant hyperbolic (point-source) reflections. Existing depositional models, based primarily on seismic data, have been constructed on the basis that this acoustic signature is indicative of ...
F. S. Stewart, M. S. Stoker
exaly   +2 more sources

Sand intraclasts within a diamicton mélange, southern Niagara Peninsula, Ontario, Canada

Journal of Quaternary Science, 1990
AbstractSand intraclasts found within diamicton units along the north shore of Lake Erie in the Mohawk Bay area of the Niagara Peninsula would appear to be part of a ‘block‐in‐matrix’ mélange. The intraclasts are undeformed and many exhibit primary bedding structures.
exaly   +2 more sources

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