Heavy mineral investigations from surface sediments of the East Greenland continental margin ...
During the expeditions ARK-VII/1, ARK-VII/3 and ARK-Xl2 sediment cores were taken by "RV Polarstern" from the shelf and the fjords of East Greenland and the Greenland Sea. The magnetic susceptibility and heavy mineral were determined at 48 surface sediment samples from undisturbed box core...
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Online Access: | https://dx.doi.org/10.1594/pangaea.701354 https://doi.pangaea.de/10.1594/PANGAEA.701354 |
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ftdatacite:10.1594/pangaea.701354 2023-12-31T10:06:21+01:00 Heavy mineral investigations from surface sediments of the East Greenland continental margin ... Grafenauer, Ingo Stein, Ruediger Fütterer, Dieter K 2008 application/zip https://dx.doi.org/10.1594/pangaea.701354 https://doi.pangaea.de/10.1594/PANGAEA.701354 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box corer Kasten corer Gravity corer Kiel type ARK-VII/1 ARK-VII/3b ARK-X/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Supplementary Publication Series of Datasets article Collection 2008 ftdatacite https://doi.org/10.1594/pangaea.701354 2023-12-01T11:07:06Z During the expeditions ARK-VII/1, ARK-VII/3 and ARK-Xl2 sediment cores were taken by "RV Polarstern" from the shelf and the fjords of East Greenland and the Greenland Sea. The magnetic susceptibility and heavy mineral were determined at 48 surface sediment samples from undisturbed box cores. The main objective of this study was the identification of source areas and transport processes of terrigenous sediments at the East Greenland continental margin. The results can be summarized as lollows:1a) Magnetic susceptibility in the North Atlantic is useful to detect delivery regions of the material transported by currents.b) The magnetic susceptibility is controlled by the ferromagnetic particles of the silt fraction.c) There are four important source areas: . The ferromagnetic particles of the box core PS2644-2 are transported from the Iceland Archipelago. . The material from the Geiki-Plateau effects the magnetic susceptibility in the Scoresby Sund Basin. . The magnetic susceptibility in the shelf regions in the ... : Supplement to: Grafenauer, Ingo (1998): Terrigener Sedimenteintrag am Ostgrönländischen Kontinentalrand - Rekonstruktion anhand von Schwermineraldaten. Diploma Thesis, Rheinisch-Westfälisch-Technische Hochschule Aachen, 94 pp ... Article in Journal/Newspaper East Greenland Greenland Greenland Sea Iceland North Atlantic Scoresby Sund DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Giant box corer Kasten corer Gravity corer Kiel type ARK-VII/1 ARK-VII/3b ARK-X/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
spellingShingle |
Giant box corer Kasten corer Gravity corer Kiel type ARK-VII/1 ARK-VII/3b ARK-X/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Grafenauer, Ingo Stein, Ruediger Fütterer, Dieter K Heavy mineral investigations from surface sediments of the East Greenland continental margin ... |
topic_facet |
Giant box corer Kasten corer Gravity corer Kiel type ARK-VII/1 ARK-VII/3b ARK-X/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
description |
During the expeditions ARK-VII/1, ARK-VII/3 and ARK-Xl2 sediment cores were taken by "RV Polarstern" from the shelf and the fjords of East Greenland and the Greenland Sea. The magnetic susceptibility and heavy mineral were determined at 48 surface sediment samples from undisturbed box cores. The main objective of this study was the identification of source areas and transport processes of terrigenous sediments at the East Greenland continental margin. The results can be summarized as lollows:1a) Magnetic susceptibility in the North Atlantic is useful to detect delivery regions of the material transported by currents.b) The magnetic susceptibility is controlled by the ferromagnetic particles of the silt fraction.c) There are four important source areas: . The ferromagnetic particles of the box core PS2644-2 are transported from the Iceland Archipelago. . The material from the Geiki-Plateau effects the magnetic susceptibility in the Scoresby Sund Basin. . The magnetic susceptibility in the shelf regions in the ... : Supplement to: Grafenauer, Ingo (1998): Terrigener Sedimenteintrag am Ostgrönländischen Kontinentalrand - Rekonstruktion anhand von Schwermineraldaten. Diploma Thesis, Rheinisch-Westfälisch-Technische Hochschule Aachen, 94 pp ... |
format |
Article in Journal/Newspaper |
author |
Grafenauer, Ingo Stein, Ruediger Fütterer, Dieter K |
author_facet |
Grafenauer, Ingo Stein, Ruediger Fütterer, Dieter K |
author_sort |
Grafenauer, Ingo |
title |
Heavy mineral investigations from surface sediments of the East Greenland continental margin ... |
title_short |
Heavy mineral investigations from surface sediments of the East Greenland continental margin ... |
title_full |
Heavy mineral investigations from surface sediments of the East Greenland continental margin ... |
title_fullStr |
Heavy mineral investigations from surface sediments of the East Greenland continental margin ... |
title_full_unstemmed |
Heavy mineral investigations from surface sediments of the East Greenland continental margin ... |
title_sort |
heavy mineral investigations from surface sediments of the east greenland continental margin ... |
publisher |
PANGAEA |
publishDate |
2008 |
url |
https://dx.doi.org/10.1594/pangaea.701354 https://doi.pangaea.de/10.1594/PANGAEA.701354 |
genre |
East Greenland Greenland Greenland Sea Iceland North Atlantic Scoresby Sund |
genre_facet |
East Greenland Greenland Greenland Sea Iceland North Atlantic Scoresby Sund |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.701354 |
_version_ |
1786838355289309184 |