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Melles, Martin (1991): Grain size fraction analysis of sediment core PS1017-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.621004, In supplement to: Melles, M (1991): Paläoglaziologie und Paläozeanographie im Spätquartär am Kontinentalrand des südlichen Weddellmeeres, Antarktis (Late Quaternary paleoglaciology and paleoceanography at the continental margin of the southern Weddell Sea, Antarctica). Berichte zur Polarforschung = Reports on Polar Research, 81, 190 pp, https://doi.org/10.2312/BzP_0081_1991

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Coverage:
Latitude: -77.243660 * Longitude: -39.145000
Date/Time Start: 1983-02-19T00:00:00 * Date/Time End: 1983-02-19T00:00:00
Minimum DEPTH, sediment/rock: 0.08 m * Maximum DEPTH, sediment/rock: 1.95 m
Event(s):
PS1017-1 (PS01/184) * Latitude: -77.243660 * Longitude: -39.145000 * Date/Time: 1983-02-19T00:00:00 * Elevation: -874.0 m * Penetration: 2.5 m * Recovery: 2.02 m * Location: Filchner Trough * Campaign: ANT-I/2 (PS01) * Basis: Polarstern * Method/Device: Giant box corer (GKG) * Comment: 3 core sections: 0-0.1, 0.1-1.1, 1.1-2.02 m
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2Size fraction 0.125-0.063 mm, 3.0-4.0 phi, very fine sand125-63 µm%Melles, MartinGrain size, sievingof sand and gravel fraction
3Size fraction 0.250-0.125 mm, 2.0-3.0 phi, fine sand250-125 µm%Melles, MartinGrain size, sievingof sand and gravel fraction
4Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand500-250 µm%Melles, MartinGrain size, sievingof sand and gravel fraction
5Size fraction 1.000-0.500 mm, 0.0-1.0 phi, coarse sand1-0.5 mm%Melles, MartinGrain size, sievingof sand and gravel fraction
6Size fraction 2.000-1.000 mm, (-1.0)-0.0 phi, very coarse sand2-1 mm%Melles, MartinGrain size, sievingof sand and gravel fraction
7Size fraction > 2 mm, gravel>2 mm%Melles, MartinGrain size, sievingof sand and gravel fraction
8Sand, mass nettoSandgMelles, Martingreater than 63 µm
9Gravel, mass nettoGravelgMelles, Martingreater than 2000 µm
Size:
160 data points

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