Fig. 2: Comparison of the number of grains counted in a sieve analysis

The distribution of ice rafted debris (IRD) is an important parameter in glaciomarine sediments. A simple method is presented allowing the determination of the IRD-content by counting the gravel fraction of the X-radiographs which are generally taken during sarnpling. In comparison with sieve analys...

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Bibliographic Details
Main Author: Grobe, Hannes
Format: Dataset
Language:English
Published: PANGAEA 1987
Subjects:
ANT-I/2
AWI_Paleo
DEPTH
sediment/rock
Gravity corer (Kiel type)
Ice rafted debris
Kapp Norvegia
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Polarstern
PS01
PS01/221
PS1021-1
SL
Stereomicroscope
incident light (Wild M7A/S)
Polarforschung
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.756793
https://doi.org/10.1594/PANGAEA.756793
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.756793
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.756793 2023-05-15T18:02:50+02:00 Fig. 2: Comparison of the number of grains counted in a sieve analysis Grobe, Hannes LATITUDE: -70.942830 * LONGITUDE: -13.653500 * DATE/TIME START: 1983-03-04T00:00:00 * DATE/TIME END: 1983-03-04T00:00:00 * MINIMUM DEPTH, sediment/rock: 5.28 m * MAXIMUM DEPTH, sediment/rock: 8.27 m 1987-02-02 text/tab-separated-values, 114 data points https://doi.pangaea.de/10.1594/PANGAEA.756793 https://doi.org/10.1594/PANGAEA.756793 en eng PANGAEA Data from left part of Fig. 2 (URI: https://doi.org/10.1594/PANGAEA.50170) https://doi.pangaea.de/10.1594/PANGAEA.756793 https://doi.org/10.1594/PANGAEA.756793 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Grobe, Hannes (1987): A simple method for the determination of ice-rafted debris in sediment cores. Polarforschung, 57(3), 123-126, https://doi.org/10.2312/polarforschung.57.3.123 ANT-I/2 AWI_Paleo DEPTH sediment/rock Gravity corer (Kiel type) Ice rafted debris Kapp Norvegia Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS01 PS01/221 PS1021-1 SL Stereomicroscope incident light (Wild M7A/S) Dataset 1987 ftpangaea https://doi.org/10.1594/PANGAEA.756793 https://doi.org/10.2312/polarforschung.57.3.123 https://doi.org/10.1594/PANGAEA.50170 2023-01-20T08:51:56Z The distribution of ice rafted debris (IRD) is an important parameter in glaciomarine sediments. A simple method is presented allowing the determination of the IRD-content by counting the gravel fraction of the X-radiographs which are generally taken during sarnpling. In comparison with sieve analyses corresponding values are obtained by both methods. However, more information can be made available in a shorter time by this method. Dataset Polarforschung PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-13.653500,-13.653500,-70.942830,-70.942830)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic ANT-I/2
AWI_Paleo
DEPTH
sediment/rock
Gravity corer (Kiel type)
Ice rafted debris
Kapp Norvegia
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Polarstern
PS01
PS01/221
PS1021-1
SL
Stereomicroscope
incident light (Wild M7A/S)
spellingShingle ANT-I/2
AWI_Paleo
DEPTH
sediment/rock
Gravity corer (Kiel type)
Ice rafted debris
Kapp Norvegia
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Polarstern
PS01
PS01/221
PS1021-1
SL
Stereomicroscope
incident light (Wild M7A/S)
Grobe, Hannes
Fig. 2: Comparison of the number of grains counted in a sieve analysis
topic_facet ANT-I/2
AWI_Paleo
DEPTH
sediment/rock
Gravity corer (Kiel type)
Ice rafted debris
Kapp Norvegia
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Polarstern
PS01
PS01/221
PS1021-1
SL
Stereomicroscope
incident light (Wild M7A/S)
description The distribution of ice rafted debris (IRD) is an important parameter in glaciomarine sediments. A simple method is presented allowing the determination of the IRD-content by counting the gravel fraction of the X-radiographs which are generally taken during sarnpling. In comparison with sieve analyses corresponding values are obtained by both methods. However, more information can be made available in a shorter time by this method.
format Dataset
author Grobe, Hannes
author_facet Grobe, Hannes
author_sort Grobe, Hannes
title Fig. 2: Comparison of the number of grains counted in a sieve analysis
title_short Fig. 2: Comparison of the number of grains counted in a sieve analysis
title_full Fig. 2: Comparison of the number of grains counted in a sieve analysis
title_fullStr Fig. 2: Comparison of the number of grains counted in a sieve analysis
title_full_unstemmed Fig. 2: Comparison of the number of grains counted in a sieve analysis
title_sort fig. 2: comparison of the number of grains counted in a sieve analysis
publisher PANGAEA
publishDate 1987
url https://doi.pangaea.de/10.1594/PANGAEA.756793
https://doi.org/10.1594/PANGAEA.756793
op_coverage LATITUDE: -70.942830 * LONGITUDE: -13.653500 * DATE/TIME START: 1983-03-04T00:00:00 * DATE/TIME END: 1983-03-04T00:00:00 * MINIMUM DEPTH, sediment/rock: 5.28 m * MAXIMUM DEPTH, sediment/rock: 8.27 m
long_lat ENVELOPE(-13.653500,-13.653500,-70.942830,-70.942830)
genre Polarforschung
genre_facet Polarforschung
op_source Supplement to: Grobe, Hannes (1987): A simple method for the determination of ice-rafted debris in sediment cores. Polarforschung, 57(3), 123-126, https://doi.org/10.2312/polarforschung.57.3.123
op_relation Data from left part of Fig. 2 (URI: https://doi.org/10.1594/PANGAEA.50170)
https://doi.pangaea.de/10.1594/PANGAEA.756793
https://doi.org/10.1594/PANGAEA.756793
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.756793
https://doi.org/10.2312/polarforschung.57.3.123
https://doi.org/10.1594/PANGAEA.50170
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