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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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 |
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ftciteseerx |
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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 |
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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 |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766015501963624448 |