Citation:

BzP_0081_1991

Name: Mineral composition of clay fraction of sediment core PS1400-1 (Table 17)
Creator: Martin Melles
Published: 1991
License: https://creativecommons.org/licenses/by/3.0/

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Related to:

Ehrmann, Werner; Grobe, Hannes; Fütterer, Dieter K (1991): Late Miocene to Holocene glacial history of east Antarctica revealed by sediments from sites 745 and 746. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 239-260, https://doi.org/10.2973/odp.proc.sr.119.208.1991

Ehrmann, Werner; Melles, Martin; Kuhn, Gerhard; Grobe, Hannes (1992): Significance of clay mineral assemblages in the Antarctic Ocean. Marine Geology, 107(4), 249-273, https://doi.org/10.1016/0025-3227(92)90075-S

Grobe, Hannes; Fütterer, Dieter K; Spieß, Volkhard (1990): Oligocene to Quaternary sedimentation processes on the Antarctic continental margin, ODP Leg 113, Site 693. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 121-131, https://doi.org/10.2973/odp.proc.sr.113.193.1990

Hambrey, Mike J; Ehrmann, Werner; Larsen, Birger (1991): Cenozoic glacial record of the Prydz Bay continental shelf, East Antarctica. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 77-132, https://doi.org/10.2973/odp.proc.sr.119.200.1991

Project(s):

Paleoenvironmental Reconstructions from Marine Sediments @ AWI (AWI_Paleo)

Coverage:

Latitude: -77.551660 * Longitude: -36.403330

Date/Time Start: 1986-01-16T08:18:00 * Date/Time End: 1986-01-16T08:18:00

Minimum DEPTH, sediment/rock: 0.75 m * Maximum DEPTH, sediment/rock: 2.77 m

Event(s):

PS1400-1 (PS08/384) * Latitude: -77.551660 * Longitude: -36.403330 * Date/Time: 1986-01-16T08:18:00 * Elevation: -1058.0 m * Penetration: 4.1 m * Recovery: 3 m * Location: Filchner Trough * Campaign: (PS08) * Basis: * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 3 core sections: 0-1.1, 1.1-2.1, 2.1-3 m

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Method/Device	Comment
1	DEPTH, sediment/rock	Depth sed	m			Geocode
2	Smectite	Sme	%	Melles, Martin	Calculated (Biscaye, 1964, PhD Thesis School of Yale University)
3	Smectite/standard ratio	Smec/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
4	Illite	Ill	%	Melles, Martin	X-ray diffraction, clay fraction
5	Illite/standard ratio	Ill/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
6	Chlorite	Chl	%	Melles, Martin	X-ray diffraction, clay fraction
7	Chlorite/standard ratio	Chl/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
8	Kaolinite	Kln	%	Melles, Martin	X-ray diffraction, clay fraction
9	Kaolinite/standard ratio	Kln/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
10	Talc/standard ratio	Tlc/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
11	Amphibole/standard ratio	Amp/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
12	Quartz/standard ratio	Qz/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
13	Feldspar/standard ratio	Fsp/std		Melles, Martin	X-ray diffraction, clay fraction	Standard=Molybdensulfid (MoS)
14	Quartz/Feldspar ratio	Qz/Fsp		Melles, Martin	Calculated

License:

Creative Commons Attribution 3.0 Unported (CC-BY-3.0)

Size:

130 data points

Data

Download dataset as tab-delimited text — use the following character encoding:

1 Depth sed [m]	2 Sme [%]	3 Smec/std	4 Ill [%]	5 Ill/std	6 Chl [%]	7 Chl/std	8 Kln [%]	9 Kln/std	10 Tlc/std	11 Amp/std	12 Qz/std	13 Fsp/std	14 Qz/Fsp
0.75	2	0.25	58	7.44	34	4.31	6	0.79	0.03	0.03	0.40	0.71	0.56
0.95	2	0.30	53	6.93	38	4.93	7	0.87	0.01	0.02	0.28	0.50	0.55
1.15	2	0.20	56	6.68	32	3.83	10	1.25	0.03	0.03	0.30	0.61	0.48
1.55	2	0.19	55	6.27	35	3.97	8	0.92	0.03	0.03	0.22	0.49	0.44
1.75	1	0.06	58	6.61	32	3.68	9	1.07	0.05	0.03	0.28	0.51	0.54
1.95	2	0.19	53	5.50	38	3.97	7	0.71	0.00	0.01	0.27	0.50	0.54
2.15	1	0.10	60	7.51	31	3.93	8	0.99	0.02	0.02	0.29	0.54	0.53
2.35	1	0.12	56	6.10	37	4.04	7	0.71	0.03	0.03	0.30	0.56	0.53
2.56	3	0.22	55	4.90	31	2.74	12	1.10	0.04	0.03	0.31	0.59	0.52
2.77	3	0.25	55	4.82	32	2.79	10	0.86	0.04	0.03	0.35	0.71	0.50