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Gamboa, Adriana; Montero-Serrano, Jean-Carlos; St-Onge, Guillaume; Rochon, André; Desiage, Pierre-Arnaud (2016): Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.866869, In supplement to: Gamboa, A et al. (2017): Mineralogical, geochemical and magnetic signatures of surface sediments from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic). Geochemistry, Geophysics, Geosystems, 18(2), 488-512, https://doi.org/10.1002/2016GC006477

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Coverage:
Median Latitude: 70.796529 * Median Longitude: -129.471412 * South-bound Latitude: 69.488000 * West-bound Longitude: -138.597000 * North-bound Latitude: 71.907000 * East-bound Longitude: -122.630000
Minimum DEPTH, sediment/rock: m * Maximum DEPTH, sediment/rock: m
Event(s):
2004-804-106 (106)  * Latitude: 70.600000 * Longitude: -122.630000 * Elevation: -122.0 m * Location: Northwestern Passages * Method/Device: Box corer (BC)
2004-804-109 (109)  * Latitude: 70.660000 * Longitude: -123.430000 * Elevation: -569.0 m * Location: Northwestern Passages * Method/Device: Box corer (BC)
2004-804-115 (115)  * Latitude: 70.849000 * Longitude: -125.050000 * Elevation: -352.0 m * Location: Northwestern Passages * Method/Device: Box corer (BC)
Comment:
For the semi-quantification of the major mineralogical components, bulk sediment XRD scans were processed in the software package X'Pert High-Score Plus (PANalytical) using the Rietveld full-pattern fitting method. This method permits the semi-quantification of whole-sediment mineralogy with a precision of 5-10% for phyllosilicates and 5% for non-phyllosilicates minerals. The quality of the Rietveld fitting procedure was evaluated for the R-profile and goodness-of-fit (GOF). The R-profile quantifies the difference between the observed and calculated patterns, whereas the GOF is the ratio between the R-weighted profile (RWP; best least-squares fit between observed and calculated patterns) and R-expected theoretical (Rexp; best possible value for the residual).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEventMontero-Serrano, Jean-Carlos
Station labelStationMontero-Serrano, Jean-Carlos
Latitude of eventLatitudeMontero-Serrano, Jean-Carlos
Longitude of eventLongitudeMontero-Serrano, Jean-Carlos
Elevation of eventElevationmMontero-Serrano, Jean-Carlos
DEPTH, sediment/rockDepth sedmMontero-Serrano, Jean-CarlosGeocode
ZoneZoneMontero-Serrano, Jean-CarlosBased on the regional morphology, mud volcanoes distribution (Blasco et al., 2013), and the influence of the Mackenzie River plume (Richerol et al., 2008; Scott et al., 2008), the surface sediment samples were divided into four main geographical areas: Mackenzie Trough-Canadian Beaufort Shelf (MT-CBS), mud volcanoes (MV), central Amundsen Gulf (cAG), and southwestern Banks Island (SWBI).
DifferenceDiffMontero-Serrano, Jean-CarlosR-profile: difference between the observed and calculated XRD patterns
Goodness of fitr**2Montero-Serrano, Jean-Carlos
10 QuartzQz%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
11 KalifeldsparKfs%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
12 PlagioclasePl%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
13 CalciteCal%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
14 DolomiteDol%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
15 PyroxenePyrox%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
16 MagnetiteFe3O4%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
17 Iron oxideFe oxide%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
18 PhyllosilicatePhyllosilicate%Montero-Serrano, Jean-CarlosX-ray diffraction (XRD)
Size:
442 data points

Data

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


Event

Station

Latitude

Longitude

Elevation [m]

Depth sed [m]

Zone

Diff

r**2
10 
Qz [%]
11 
Kfs [%]
12 
Pl [%]
13 
Cal [%]
14 
Dol [%]
15 
Pyrox [%]
16 
Fe3O4 [%]
17 
Fe oxide [%]
18 
Phyllosilicate [%]
2004-804-106 10670.6000-122.6300-1220cAG21.82.261.53.27.00.211.90.40.00.614.7
2004-804-109 10970.6600-123.4300-5690cAG23.32.229.410.15.00.314.60.00.31.136.4
2004-804-115 11570.8490-125.0500-3520cAG24.32.436.34.96.50.226.00.00.40.421.7
2004-804-118 11870.9440-125.8500-3880cAG24.72.430.15.96.90.28.10.10.50.841.2
2004-804-124 12471.3900-126.7190-4420cAG23.82.130.07.95.40.09.10.00.51.239.4
2004-804-200 20070.0450-126.2970-2360CBS24.32.532.36.85.70.24.60.50.31.143.9
2004-804-206 20670.3210-124.8390-950cAG25.52.932.66.36.70.28.90.00.51.042.3
2004-804-209 20970.5390-124.3660-2410cAG24.72.634.49.25.50.013.50.40.30.834.8
2004-804-212 21270.7570-123.8900-4300SWBI24.02.428.28.15.30.228.30.90.10.724.3
2004-804-215 21570.9740-123.4150-2970SWBI23.12.134.97.76.30.134.80.30.20.215.1
2004-804-250 25070.4520-125.4230-1930CBS26.53.032.06.66.20.24.60.00.41.247.6
2004-804-309 30971.1250-125.8340-3970cAG25.22.532.77.56.70.19.90.10.30.841.5
2004-804-312 31271.3020-125.1920-3070SWBI22.62.132.48.84.90.025.30.70.40.726.7
2004-804-315 31571.4860-124.5430-2240SWBI23.42.231.28.44.50.021.90.00.40.727.8
2004-804-400 40070.9170-128.9330-360MV24.32.539.66.07.50.39.40.40.20.835.3
2004-804-403 40371.1130-128.3050-590MV23.02.559.82.86.80.07.00.60.20.620.8
2004-804-406 40671.3110-127.6990-1790CBS25.12.734.88.25.70.35.90.30.40.742.7
2004-804-409 40971.5120-127.0920-3870cAG24.62.431.19.86.50.29.90.20.41.140.0
2004-804-412 41271.7000-126.4770-3900SWBI24.12.334.17.76.20.019.20.00.30.931.2
2004-804-415 41571.9070-125.8680-560SWBI22.52.135.67.56.20.133.90.00.10.515.8
2004-804-609 60970.9430-130.5230-440MV22.42.251.74.08.80.16.30.00.20.427.9
2004-804-650 65071.3090-131.6190-2410CBS25.32.738.08.56.30.34.50.00.31.140.2
2004-804-709 70970.9640-133.7840-870MV21.62.263.62.911.30.24.40.00.20.316.7
2004-804-711 71170.8240-133.8030-770CBS26.53.035.86.87.80.45.70.50.40.841.4
2004-804-712 71270.6900-133.6810-700CBS26.12.938.36.95.60.13.70.00.61.143.2
2004-804-718 71870.1700-133.5340-450CBS25.62.733.35.94.90.02.70.00.41.745.1
2004-804-750 75071.3460-134.1440-10870CBS25.02.633.67.46.60.02.80.00.71.243.1
2004-804-803 80370.6360-135.9170-2370CBS24.92.731.97.34.60.03.70.70.21.047.1
2004-804-805A 80570.3930-135.4200-660MV24.12.743.44.210.11.35.60.80.20.432.7
2004-804-809 80970.0950-135.3410-420CBS25.52.832.68.04.40.23.30.00.51.047.9
2004-804-850 85070.5480-137.6000-10710CBS25.52.634.57.35.20.02.80.20.61.544.5
2004-804-906 90670.0190-138.5970-2720CBS25.22.735.05.67.60.23.60.20.50.745.9
2004-804-909 90969.7530-138.2720-1690CBS24.32.635.15.37.40.44.40.90.40.844.7
2004-804-912 91269.4880-137.9410-540CBS25.02.536.35.26.10.73.91.00.41.241.6