Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Andrews, John T; Stein, Ruediger; Moros, Matthias; Perner, Kerstin (2016): XRD mineralogy of sediment core PS2630-5 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.848753, In supplement to: Andrews, JT et al. (2016): Late Quaternary changes in sediment composition on the NE Greenland margin (~73° N) with a focus on the fjords and shelf. Boreas, https://doi.org/10.1111/bor.12169

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Further details:
Eberl, Dennis D (2003): User's guide to RockJock - A program for determining quantitative mineralogy from powder X-ray diffraction data. U.S. Geological Survey Open-File Report 2003-78, 47 pp, https://pubs.usgs.gov/of/2003/of03-078/
Eberl, Dennis D (2004): Quantitative mineralogy of the Yukon River system: Changes with reach and season, and determining sediment provenance. American Mineralogist, 89, 1784-1794, https://pubs.usgs.gov/publication/70026557
Coverage:
Latitude: 73.158330 * Longitude: -18.068330
Date/Time Start: 1994-09-03T22:23:00 * Date/Time End: 1994-09-03T22:23:00
Minimum DEPTH, sediment/rock: 0.100 m * Maximum DEPTH, sediment/rock: 2.900 m
Event(s):
PS2630-5 (PS31/138) * Latitude: 73.158330 * Longitude: -18.068330 * Date/Time: 1994-09-03T22:23:00 * Elevation: -287.0 m * Penetration: 5 m * Recovery: 3.02 m * Location: East Greenland Sea * Campaign: ARK-X/2 (PS31) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 4 core sections: 0-0.29, 0.29-1.02, 1.02-2.02, 2.02-3.02 m
Comment:
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are scanned on a D5000 Siemens X-Ray Diffractometer between 5° and 65° 2-theta with a 0.02° step and a 2-sec count. The resulting 3000 data points are loaded into the Excel macro-program Rockjock v6 (Eberl, 2003) and the weight% of minerals in the sediment mixtures calculated against a suite of 124 "standard" mineral patterns (Eberl, 2003). Finally, the data are normalized to sum to 100%
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmAndrews, John TGeocode
Full pattern degree of fitPatt deg fitAndrews, John T
QuartzQz%Andrews, John TX-ray diffraction (Siemens D5000)
MicroclineMc%Andrews, John TX-ray diffraction (Siemens D5000)ordered
MicroclineMc%Andrews, John TX-ray diffraction (Siemens D5000)intermediate
OrthoclaseOr%Andrews, John TX-ray diffraction (Siemens D5000)
AnorthoclaseAnor%Andrews, John TX-ray diffraction (Siemens D5000)
AlbiteAb%Andrews, John TX-ray diffraction (Siemens D5000)Cleavelandite
OligoclaseOligoc%Andrews, John TX-ray diffraction (Siemens D5000)Norway
10 LabradoriteLab%Andrews, John TX-ray diffraction (Siemens D5000)
11 BytowniteByt%Andrews, John TX-ray diffraction (Siemens D5000)
12 AnorthiteAn%Andrews, John TX-ray diffraction (Siemens D5000)
13 CalciteCal%Andrews, John TX-ray diffraction (Siemens D5000)
14 DolomiteDol%Andrews, John TX-ray diffraction (Siemens D5000)
15 Iron-DolomiteFe-Dol%Andrews, John TX-ray diffraction (Siemens D5000)
16 SideriteSd%Andrews, John TX-ray diffraction (Siemens D5000)
17 HaliteHl%Andrews, John TX-ray diffraction (Siemens D5000)
18 FerrotschermakiteFts%Andrews, John TX-ray diffraction (Siemens D5000)
19 DiopsideDi%Andrews, John TX-ray diffraction (Siemens D5000)
20 Pyrite, FeS2Py%Andrews, John TX-ray diffraction (Siemens D5000)
21 MagnetiteFe3O4%Andrews, John TX-ray diffraction (Siemens D5000)
22 Hematite, Fe2O3Hem%Andrews, John TX-ray diffraction (Siemens D5000)
23 MaghemiteMgh%Andrews, John TX-ray diffraction (Siemens D5000)
24 DiatomsDiatoms%Andrews, John TX-ray diffraction (Siemens D5000)
25 ChertChert%Andrews, John TX-ray diffraction (Siemens D5000)8.4 nm
26 Non-clay mineralsNon-clay min%Andrews, John TX-ray diffraction (Siemens D5000)
27 KaoliniteKln%Andrews, John TX-ray diffraction (Siemens D5000)dry branch
28 SaponiteSap%Andrews, John TX-ray diffraction (Siemens D5000)
29 SmectiteSme%Andrews, John TX-ray diffraction (Siemens D5000)ferruginous
30 IlliteIll%Andrews, John TX-ray diffraction (Siemens D5000)1Md +dioct. mica & smectite
31 IlliteIll%Andrews, John TX-ray diffraction (Siemens D5000)1M R>2 88 %I
32 IlliteIll%Andrews, John TX-ray diffraction (Siemens D5000)1M R>1 70-80 %I
33 BiotiteBt%Andrews, John TX-ray diffraction (Siemens D5000)1M
34 Iron-ChloriteFe chl%Andrews, John TX-ray diffraction (Siemens D5000)Tusc
35 MuscoviteMs%Andrews, John TX-ray diffraction (Siemens D5000)2M1
36 IlliteIll%Andrews, John TX-ray diffraction (Siemens D5000)1M PD3B
37 Clay mineralsClay min%Andrews, John TX-ray diffraction (Siemens D5000)
38 TotalTotal%Andrews, John TX-ray diffraction (Siemens D5000)
Size:
1036 data points

Data

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


Depth sed [m]

Patt deg fit

Qz [%]

Mc [%]
(ordered)

Mc [%]
(intermediate)

Or [%]

Anor [%]

Ab [%]
(Cleavelandite)

Oligoc [%]
(Norway)
10 
Lab [%]
11 
Byt [%]
12 
An [%]
13 
Cal [%]
14 
Dol [%]
15 
Fe-Dol [%]
16 
Sd [%]
17 
Hl [%]
18 
Fts [%]
19 
Di [%]
20 
Py [%]
21 
Fe3O4 [%]
22 
Hem [%]
23 
Mgh [%]
24 
Diatoms [%]
25 
Chert [%]
(8.4 nm)
26 
Non-clay min [%]
27 
Kln [%]
(dry branch)
28 
Sap [%]
29 
Sme [%]
(ferruginous)
30 
Ill [%]
(1Md +dioct. mica & smectite)
31 
Ill [%]
(1M R>2 88 %I)
32 
Ill [%]
(1M R>1 70-80 %I)
33 
Bt [%]
(1M)
34 
Fe chl [%]
(Tusc)
35 
Ms [%]
(2M1)
36 
Ill [%]
(1M PD3B)
37 
Clay min [%]
38 
Total [%]
0.1000.08915.50.05.80.08.24.02.02.90.60.21.00.51.00.90.00.10.20.30.00.21.93.811.059.93.18.22.04.64.34.83.53.04.81.940.1100
0.2000.09727.80.04.90.08.23.92.94.70.80.02.80.11.70.90.00.62.20.40.00.21.12.39.975.11.73.40.71.83.33.22.63.24.40.524.9100
0.3000.08716.90.04.70.09.43.62.24.12.60.22.10.11.60.90.00.32.20.30.00.32.03.18.364.92.76.52.83.15.32.42.04.45.00.835.1100
0.4000.09427.72.24.70.09.14.43.63.70.00.02.30.02.80.40.10.81.40.40.00.11.02.810.077.40.94.41.90.03.52.72.03.63.70.022.6100
0.5000.12320.80.05.70.39.05.93.53.50.00.03.50.81.60.60.00.81.50.20.00.21.30.27.066.71.34.62.00.04.44.73.35.77.10.233.3100
0.6000.08925.91.15.80.19.13.94.22.10.50.02.60.11.40.50.00.81.40.20.00.20.51.87.970.11.05.62.40.03.83.32.95.35.40.129.9100
0.7000.09015.20.05.10.17.84.63.92.02.30.53.40.01.70.30.01.41.80.10.00.31.20.111.863.52.04.02.21.83.13.54.85.99.00.136.5100
0.8000.09218.80.05.90.47.34.13.82.10.01.92.70.11.50.20.00.91.10.00.00.32.20.013.967.41.33.62.80.43.33.84.66.36.50.032.6100
0.9000.09113.30.05.20.08.04.43.23.00.50.92.90.01.90.60.00.31.20.20.00.21.60.312.660.61.74.93.10.94.65.14.36.28.20.339.4100
1.0000.09617.40.05.20.010.83.70.33.82.52.33.80.01.50.90.00.12.60.30.00.13.20.010.268.92.44.04.90.05.21.72.64.26.30.131.1100
1.1000.09714.60.64.40.05.74.31.35.40.90.92.10.01.40.40.10.11.60.20.00.11.80.010.656.63.05.26.41.79.63.53.05.75.20.043.4100
1.2000.11223.92.24.12.38.75.33.73.60.00.03.70.02.20.80.01.31.10.20.00.21.10.312.176.90.12.74.50.04.83.32.63.71.40.023.1100
1.3000.08916.60.04.40.010.24.61.93.92.70.82.50.11.80.50.00.72.30.20.00.31.80.010.365.41.74.25.00.25.83.03.05.06.80.034.6100
1.4000.09018.00.04.60.010.14.10.33.92.52.02.10.00.80.70.10.02.80.30.00.22.20.010.965.33.05.15.50.16.12.02.74.75.80.034.8100
1.5000.08717.30.05.40.05.54.70.85.93.61.11.30.20.70.90.00.02.70.30.00.22.51.37.862.03.34.44.31.66.52.92.35.37.00.438.0100
1.6000.10120.70.05.10.26.33.41.04.12.72.02.00.01.10.70.00.03.40.20.00.33.50.28.465.42.36.05.10.95.71.72.35.25.50.034.6100
1.7000.08914.70.04.70.010.64.80.42.81.11.42.40.01.40.90.00.81.50.40.00.42.50.810.261.83.15.66.00.96.62.52.75.25.50.038.2100
1.8000.09321.10.35.70.07.27.23.52.10.00.03.80.51.50.20.00.81.30.10.00.31.10.012.068.60.01.24.00.02.65.44.34.49.60.031.4100
1.9000.10423.30.56.30.15.76.66.20.00.00.04.10.41.80.50.00.31.00.20.00.30.00.08.165.20.03.31.80.01.78.14.55.210.10.034.8100
2.0000.10433.41.15.70.14.16.05.41.90.00.03.70.11.60.40.00.91.20.00.00.20.00.512.478.80.00.20.60.00.05.03.94.27.30.021.2100
2.1000.10918.40.06.40.05.06.35.32.00.00.04.50.02.20.40.00.40.80.20.00.30.21.414.568.50.03.21.50.00.66.14.85.310.00.031.5100
2.2000.09332.30.95.40.15.75.64.62.70.00.23.60.01.60.40.00.71.30.10.00.20.40.713.279.90.01.40.70.00.03.73.83.76.80.020.1100
2.3000.11017.50.06.10.06.96.73.01.80.00.04.70.02.30.60.00.51.20.20.00.10.80.114.867.40.02.80.90.00.86.25.15.511.20.032.6100
2.4000.11332.90.75.21.66.18.04.51.90.40.03.30.01.70.60.00.90.80.00.00.30.00.011.280.00.01.00.40.00.03.93.83.97.00.020.0100
2.5000.10321.40.06.20.06.96.75.20.80.00.04.50.02.10.70.00.50.90.20.00.30.80.214.271.60.02.70.70.00.15.44.85.09.70.028.4100
2.6000.12423.80.66.00.08.56.62.31.70.00.03.70.01.70.00.20.11.30.20.00.20.00.119.776.70.00.10.30.00.14.45.64.97.90.023.3100
2.8000.09818.50.65.30.08.36.74.00.00.40.24.30.02.30.30.10.61.20.10.00.20.30.016.069.30.01.81.00.61.75.05.25.210.30.030.7100
2.9000.09123.40.96.10.06.95.64.42.50.00.03.30.02.10.30.00.70.90.20.00.21.21.09.569.10.14.42.20.03.84.83.25.37.00.030.9100