Soft sediment deformation structures in Silurian turbidites from North Greenland

Turbidite beds in the Silurian turbidite sequence, North Greenland, show soft sediment deformation struc-tures suggesting that the structureless (in respect of traction structures) sandstones divisions of the turbidi-tes were deposited by direct suspension sedimentation from high-density flows. The...

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Main Author: Poul-henrik Larsen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.2754
http://2dgf.dk/xpdf/bull35_01-02-19-23.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.561.2754 2023-05-15T16:26:34+02:00 Soft sediment deformation structures in Silurian turbidites from North Greenland Poul-henrik Larsen The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.2754 http://2dgf.dk/xpdf/bull35_01-02-19-23.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.2754 http://2dgf.dk/xpdf/bull35_01-02-19-23.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull35_01-02-19-23.pdf text ftciteseerx 2016-01-08T12:03:18Z Turbidite beds in the Silurian turbidite sequence, North Greenland, show soft sediment deformation struc-tures suggesting that the structureless (in respect of traction structures) sandstones divisions of the turbidi-tes were deposited by direct suspension sedimentation from high-density flows. The deposits may have re-sulted from multiple successive depositional events within the same turbidity flow. Reworking and shear-ing of the newly formed loosely packed high-density suspension deposits caused by the still moving flow above create secondary soft sediment deformation structures which may be used as current indicators if other structures are absent (e.g. flute casts). Text Greenland North Greenland Unknown Greenland
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Turbidite beds in the Silurian turbidite sequence, North Greenland, show soft sediment deformation struc-tures suggesting that the structureless (in respect of traction structures) sandstones divisions of the turbidi-tes were deposited by direct suspension sedimentation from high-density flows. The deposits may have re-sulted from multiple successive depositional events within the same turbidity flow. Reworking and shear-ing of the newly formed loosely packed high-density suspension deposits caused by the still moving flow above create secondary soft sediment deformation structures which may be used as current indicators if other structures are absent (e.g. flute casts).
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Poul-henrik Larsen
spellingShingle Poul-henrik Larsen
Soft sediment deformation structures in Silurian turbidites from North Greenland
author_facet Poul-henrik Larsen
author_sort Poul-henrik Larsen
title Soft sediment deformation structures in Silurian turbidites from North Greenland
title_short Soft sediment deformation structures in Silurian turbidites from North Greenland
title_full Soft sediment deformation structures in Silurian turbidites from North Greenland
title_fullStr Soft sediment deformation structures in Silurian turbidites from North Greenland
title_full_unstemmed Soft sediment deformation structures in Silurian turbidites from North Greenland
title_sort soft sediment deformation structures in silurian turbidites from north greenland
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.2754
http://2dgf.dk/xpdf/bull35_01-02-19-23.pdf
geographic Greenland
geographic_facet Greenland
genre Greenland
North Greenland
genre_facet Greenland
North Greenland
op_source http://2dgf.dk/xpdf/bull35_01-02-19-23.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.2754
http://2dgf.dk/xpdf/bull35_01-02-19-23.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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