Mineral and grain size data for sediment core MD99-2317 ...

Core MD99-2317 was taken from the Grivel Basin, East Greenland ) (68.103°N, 27.8615°W, 536 m wd, 25.07 m long), offshore from the 60,000 km2 early Tertiary basalt outcrop, and from an area subjected to the transport of icebergs from local and regional tidewater glaciers. Radiocarbon dates for this c...

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Main Author: Andrews, John T
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2022
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.940546
https://doi.pangaea.de/10.1594/PANGAEA.940546
id ftdatacite:10.1594/pangaea.940546
record_format openpolar
spelling ftdatacite:10.1594/pangaea.940546 2024-03-31T07:52:30+00:00 Mineral and grain size data for sediment core MD99-2317 ... Andrews, John T 2022 application/zip https://dx.doi.org/10.1594/pangaea.940546 https://doi.pangaea.de/10.1594/PANGAEA.940546 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2019.105902 https://dx.doi.org/10.1016/j.quascirev.2011.01.016 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 paired samples across a core sortable silt & ice rafted debris X-ray diffraction mineral wt% Calypso Corer MD114 Marion Dufresne 1995 article Bundled Publication of Datasets Collection 2022 ftdatacite https://doi.org/10.1594/pangaea.94054610.1016/j.quascirev.2019.10590210.1016/j.quascirev.2011.01.016 2024-03-04T13:56:14Z Core MD99-2317 was taken from the Grivel Basin, East Greenland ) (68.103°N, 27.8615°W, 536 m wd, 25.07 m long), offshore from the 60,000 km2 early Tertiary basalt outcrop, and from an area subjected to the transport of icebergs from local and regional tidewater glaciers. Radiocarbon dates for this core are reported in Jennings et al (2011). Grain size analysis of the < 2mm sediment fraction was undertaken using the Malvern 3000 master-sizer and is reported as volume% of sediment in 100 intervals between 0.01 and 3500 µm (Table 1). Derived parameters from these values (Table 2) include measures of coast sand attributed to iceberg rafting (> 240 µm), volume % of sand, and measures of the sortable silt % and the mean sortable silt grain size, which can be correlated with changes in the flow speed of bottom currents . Tables 3 and 4 report replicate runs on X-ray diffraction estimates of mineral weight % and Malvern-based grain size volume % for a series of 7 paired samples (A versus B) taken across the ... Article in Journal/Newspaper East Greenland Greenland DataCite Metadata Store (German National Library of Science and Technology) Greenland Jennings ENVELOPE(72.556,72.556,-70.145,-70.145)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic paired samples across a core
sortable silt & ice rafted debris
X-ray diffraction mineral wt%
Calypso Corer
MD114
Marion Dufresne 1995
spellingShingle paired samples across a core
sortable silt & ice rafted debris
X-ray diffraction mineral wt%
Calypso Corer
MD114
Marion Dufresne 1995
Andrews, John T
Mineral and grain size data for sediment core MD99-2317 ...
topic_facet paired samples across a core
sortable silt & ice rafted debris
X-ray diffraction mineral wt%
Calypso Corer
MD114
Marion Dufresne 1995
description Core MD99-2317 was taken from the Grivel Basin, East Greenland ) (68.103°N, 27.8615°W, 536 m wd, 25.07 m long), offshore from the 60,000 km2 early Tertiary basalt outcrop, and from an area subjected to the transport of icebergs from local and regional tidewater glaciers. Radiocarbon dates for this core are reported in Jennings et al (2011). Grain size analysis of the < 2mm sediment fraction was undertaken using the Malvern 3000 master-sizer and is reported as volume% of sediment in 100 intervals between 0.01 and 3500 µm (Table 1). Derived parameters from these values (Table 2) include measures of coast sand attributed to iceberg rafting (> 240 µm), volume % of sand, and measures of the sortable silt % and the mean sortable silt grain size, which can be correlated with changes in the flow speed of bottom currents . Tables 3 and 4 report replicate runs on X-ray diffraction estimates of mineral weight % and Malvern-based grain size volume % for a series of 7 paired samples (A versus B) taken across the ...
format Article in Journal/Newspaper
author Andrews, John T
author_facet Andrews, John T
author_sort Andrews, John T
title Mineral and grain size data for sediment core MD99-2317 ...
title_short Mineral and grain size data for sediment core MD99-2317 ...
title_full Mineral and grain size data for sediment core MD99-2317 ...
title_fullStr Mineral and grain size data for sediment core MD99-2317 ...
title_full_unstemmed Mineral and grain size data for sediment core MD99-2317 ...
title_sort mineral and grain size data for sediment core md99-2317 ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.940546
https://doi.pangaea.de/10.1594/PANGAEA.940546
long_lat ENVELOPE(72.556,72.556,-70.145,-70.145)
geographic Greenland
Jennings
geographic_facet Greenland
Jennings
genre East Greenland
Greenland
genre_facet East Greenland
Greenland
op_relation https://dx.doi.org/10.1016/j.quascirev.2019.105902
https://dx.doi.org/10.1016/j.quascirev.2011.01.016
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.94054610.1016/j.quascirev.2019.10590210.1016/j.quascirev.2011.01.016
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