Citation:

PANGAEA.962728

Name: Mineral composition of samples from sediment cores from cruise HU90023
Published: 2023-11-01
License: https://creativecommons.org/licenses/by/4.0/
Keywords: Hudson Strait,; Labrador Sea; Mineral compositions; Sediment unmixing; X-ray diffraction

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Keyword(s):

Hudson Strait,; Labrador Sea; Mineral compositions; Sediment unmixing; X-ray diffraction

References:

Maclean, B (1991): Cruise Report - Css Hudson Cruise 90-023: Marine Geological Investigations in Hudson Strait, Ungava Bay, and Frobisher Bay. Atlantic Geoscience Centre. Geological Survey of Canada, 157 pp, https://doi.org/10.4095/132381

Maclean, B (2001): Bedrock geology of Hudson Strait and Ungava Bay. In: MacLean , B. (ed.), Marine Geology of Hudson Strait and Ungava Bay, Eastern Arctic Canada: Late Quaternary Sediments, Depositional Environments, and Late Glacial-Deglacial History derived from Marine and Terrestrial studies. Queen's Printer, Ottawa, 65-69

Maclean, B (2001): Late Quaternary Sediments, Depositional Environments, and Late Glacial-Deglacial History derived from Marine and Terrestrial studies. Queen's Printer, Ottawa, 5-17

Coverage:

Median Latitude: 61.833429 * Median Longitude: -70.334286 * South-bound Latitude: 59.990000 * West-bound Longitude: -81.988000 * North-bound Latitude: 63.066000 * East-bound Longitude: -63.876000

Minimum DEPTH, sediment/rock: 0.55 m * Maximum DEPTH, sediment/rock: 7.01 m

Event(s):

HU90-023-030 * Latitude: 61.782000 * Longitude: -63.876000 * Elevation: -572.0 m * Location: Hudson Strait * Campaign: * Basis: Hudson * Method/Device: Piston corer (PC)

HU90-023-031 * Latitude: 60.951000 * Longitude: -65.733000 * Elevation: -872.0 m * Location: Hudson Strait * Campaign: * Basis: Hudson * Method/Device: Piston corer (PC)

HU90-023-034 * Latitude: 59.990000 * Longitude: -65.733000 * Elevation: -112.0 m * Location: Hudson Strait * Campaign: * Basis: Hudson * Method/Device: Piston corer (PC)

Comment:

Samples from six piston cores from cruise HU90023-030, -031, -034, -045, 099 and 101 (MacLean, 1991) were processed to provide information of the source(s) of Hudson Strait Heinrich sediments in the Labrador Sea. The cores are located in terms of latitude, longitude, water depth, and the regional name for each site (MacLean, 2001a). Radiocarbon dates on the cores are listed in MacLean (ed) (2001) and in (Manley and Jennings, 1996).

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Comment
1	Event label	Event		Andrews, John T
2	Latitude of event	Latitude		Andrews, John T
3	Longitude of event	Longitude		Andrews, John T
4	Elevation of event	Elevation	m	Andrews, John T
5	DEPTH, sediment/rock	Depth sed	m	Andrews, John T	Geocode
6	Full pattern degree of fit	Patt deg fit		Andrews, John T
7	Quartz	Qz	%	Andrews, John T
8	Microcline	Mc	%	Andrews, John T	ordered Microcline feldspar
9	Microcline	Mc	%	Andrews, John T	intermediate Microcline feldspar
10	Orthoclase	Or	%	Andrews, John T
11	Anorthoclase	Anor	%	Andrews, John T
12	Albite	Ab	%	Andrews, John T	Albite feldspar (Cleavelandite)
13	Oligoclase	Oligoc	%	Andrews, John T	Oligoclase feldspar (Norway)
14	Labradorite	Lab	%	Andrews, John T
15	Bytownite	Byt	%	Andrews, John T
16	Anorthite	An	%	Andrews, John T
17	Calcite	Cal	%	Andrews, John T
18	Dolomite	Dol	%	Andrews, John T
19	Iron-Dolomite	Fe-Dol	%	Andrews, John T
20	Siderite	Sd	%	Andrews, John T
21	Halite	Hl	%	Andrews, John T
22	Ferrotschermakite	Fts	%	Andrews, John T
23	Diopside	Di	%	Andrews, John T
24	Pyrite, FeS2	Py	%	Andrews, John T
25	Magnetite	Fe3O4	%	Andrews, John T
26	Hematite, Fe2O3	Hem	%	Andrews, John T
27	Maghemite	Mgh	%	Andrews, John T
28	Diatoms	Diatoms	%	Andrews, John T
29	Chert	Chert	%	Andrews, John T	8.4 nm
30	Non-clay minerals	Non-clay min	%	Andrews, John T
31	Kaolinite	Kln	%	Andrews, John T	Kaolinite (Dry Branch)
32	Saponite	Sap	%	Andrews, John T
33	Ferruginous smectite	Fe-sme	%	Andrews, John T
34	Illite	Ill	%	Andrews, John T	1Md illite (+ dioct mica & smectite)
35	Illite	Ill	%	Andrews, John T	1M Illite (R>2; 88%I)
36	Illite	Ill	%	Andrews, John T	1M illite (R>1, 70-80%I)
37	Biotite	Bt	%	Andrews, John T	Biotite (1M)
38	Iron-Chlorite	Fe chl	%	Andrews, John T	Fe-Chlorite (Tusc)
39	Muscovite	Ms	%	Andrews, John T	Muscovite (2M1)
40	Illite	Ill	%	Andrews, John T	Illite (1M, PD3B)
41	Clay minerals	Clay min	%	Andrews, John T	total

License:

Creative Commons Attribution 4.0 International (CC-BY-4.0)

Status:

Curation Level: Enhanced curation (CurationLevelC)

Size:

1719 data points

Data

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

1 Event	2 Latitude	3 Longitude	4 Elevation [m]	5 Depth sed [m]	6 Patt deg fit	7 Qz [%]	8 Mc [%] (ordered Microcline feldspar)	9 Mc [%] (intermediate Microcline feldspar)	10 Or [%]	11 Anor [%]	12 Ab [%] (Albite feldspar (Cleavelandite))	13 Oligoc [%] (Oligoclase feldspar (Norway))	14 Lab [%]	15 Byt [%]	16 An [%]	17 Cal [%]	18 Dol [%]	19 Fe-Dol [%]	20 Sd [%]	21 Hl [%]	22 Fts [%]	23 Di [%]	24 Py [%]	25 Fe3O4 [%]	26 Hem [%]	27 Mgh [%]	28 Diatoms [%]	29 Chert [%] (8.4 nm)	30 Non-clay min [%]	31 Kln [%] (Kaolinite (Dry Branch))	32 Sap [%]	33 Fe-sme [%]	34 Ill [%] (1Md illite (+ dioct mica & sm...)	35 Ill [%] (1M Illite (R>2; 88%I))	36 Ill [%] (1M illite (R>1, 70-80%I))	37 Bt [%] (Biotite (1M))	38 Fe chl [%] (Fe-Chlorite (Tusc))	39 Ms [%] (Muscovite (2M1))	40 Ill [%] (Illite (1M, PD3B))	41 Clay min [%] (total)
HU90-023-030	61.7820	-63.8760	-572	2.52	0.1258	11.9		7.0	2.2		0.5	6.1	3.8	0.0	0.0	38.6	0.0	11.7	0.4	0.0	0.7	0.0	0.1	0.0	0.0	0.0	0.0		85.0	0.0	0.9	3.0	1.9			5.0	2.2	1.6	0.4	15.0
HU90-023-030	61.7820	-63.8760	-572	5.23	0.0875	13.4		8.7	3.2		1.0	11.9	7.2	0.0	0.7	10.1	0.3	6.4	0.4	0.0	1.5	0.0	0.3	0.0	0.0	0.0	0.0		66.0	0.0	4.3	8.7	3.4			9.1	5.2	3.3	0.0	34.0
HU90-023-030	61.7820	-63.8760	-572	6.24	0.1120	12.8		8.5	3.3		2.2	10.2	6.7	0.0	0.0	8.1	0.5	7.2	1.0	0.2	2.3	0.0	0.4	0.0	0.1	0.0	0.0		65.0	0.0	4.0	6.0	5.3			10.8	6.9	2.0	0.0	35.0
HU90-023-030	61.7820	-63.8760	-572	0.61	0.1407	9.6		8.7	2.0		0.0	5.7	3.7	0.0	0.0	36.0	0.0	10.8	0.8	0.0	0.6	0.0	0.2	0.0	0.1	0.7	0.0		80.8	0.0	1.3	0.0	4.5			4.4	6.6	1.5	0.8	19.3
HU90-023-031	60.9510	-65.7330	-872	0.55	0.1163	32.1		9.9	2.1		3.2	7.3	4.6	0.0	1.4	14.0	0.0	8.8	0.1	0.2	0.7	0.0	0.3	0.0	0.2	0.0	0.0		85.9	0.0	1.0	2.6	1.7			4.3	2.5	1.9	0.0	14.1
HU90-023-031	60.9510	-65.7330	-872	1.03	0.1144	37.0		9.8	1.5		2.3	7.7	3.7	0.0	0.7	13.1	0.0	7.1	0.3	0.1	1.6	0.0	0.2	0.0	0.1	0.0	0.0		86.8	0.0	0.5	1.2	1.7			5.4	2.6	1.7	0.0	13.2
HU90-023-031	60.9510	-65.7330	-872	3.56	0.1182	32.0		9.7	1.9		2.8	7.3	4.1	0.0	0.0	14.3	0.8	8.4	0.5	0.0	1.8	0.0	0.1	0.0	0.2	0.1	0.0		85.7	0.0	0.4	1.7	1.8			5.6	2.8	1.9	0.0	14.3
HU90-023-031	60.9510	-65.7330	-872	4.56	0.1108	37.5		10.1	2.9		1.9	7.6	3.1	0.0	0.9	13.3	0.0	8.7	0.4	0.0	1.4	0.0	0.0	0.0	0.0	0.0	0.0		88.9	0.0	0.2	0.2	1.8			5.1	2.8	1.1	0.0	11.1
HU90-023-031	60.9510	-65.7330	-872	7.01	0.1388	46.8		11.2	2.3		1.2	8.7	3.4	0.0	0.2	9.0	0.3	5.7	0.5	0.0	1.1	0.0	0.1	0.0	0.1	0.4	0.0		91.8	0.0	0.3	0.0	1.1			3.6	2.5	0.7	0.0	8.2
HU90-023-034	59.9900	-65.7330	-112	1.40	0.1003	9.8	2.6	5.5	0.0	3.3	9.4	10.8	0.8	0.0	0.0	1.6	0.1	2.2	0.1	0.6	3.8	0.0	0.0	0.0	0.3	2.1	4.3	4.8	62.1	0.0	9.0	1.9	3.2	1.0	6.5	3.6	8.5	4.2	0.0	37.9
HU90-023-034	59.9900	-65.7330	-112	1.54	0.0948	11.0	2.0	6.0	0.0	2.2	6.9	10.0	3.1	0.0	0.0	5.4	0.0	3.7	0.4	0.4	3.4	0.4	0.0	0.0	0.2	1.3	3.5	2.7	62.5	0.0	7.8	0.1	2.6	0.0	7.1	5.9	10.4	3.5	0.0	37.5
HU90-023-034	59.9900	-65.7330	-112	1.17	0.1026	12.1	1.5	5.8	0.0	4.9	7.0	10.4	2.6	0.0	0.0	2.8	0.0	2.8	0.5	0.2	4.3	0.1	0.0	0.3	0.2	2.0	3.6	3.5	64.8	0.0	7.8	0.0	3.4	0.0	4.6	6.5	9.7	3.3	0.0	35.2
HU90-023-034	59.9900	-65.7330	-112	1.41	0.1002	11.7	2.1	5.4	0.0	4.7	7.0	10.9	1.6	0.0	0.0	2.7	0.0	3.1	0.5	0.3	4.0	0.2	0.0	0.4	0.4	1.1	3.0	2.0	61.0	0.0	6.4	0.0	3.6	0.0	6.6	8.0	10.6	3.8	0.0	39.0
HU90-023-034	59.9900	-65.7330	-112	1.47	0.0863	10.0	1.7	5.8	0.2	4.8	3.9	9.0	1.2	0.0	0.2	11.2	1.2	6.7	0.2	0.2	2.4	0.4	0.0	0.4	0.1	0.7	3.3	2.3	65.7	0.0	3.9	0.0	2.6	0.0	5.8	8.0	10.3	3.7	0.0	34.3
HU90-023-045	60.9500	-66.1400	-845	4.16	0.0959	23.8	3.7	3.3	1.7	7.9	3.6	6.1	3.4	0.0	0.0	12.4	3.5	5.7	0.4	0.0	1.9	0.5	0.2	0.0	0.0	1.6	3.2	3.9	86.7	0.0	3.9	1.1	0.0	0.0	2.8	3.4	1.8	0.3	0.0	13.3
HU90-023-045	60.9500	-66.1400	-845	4.66	0.0883	20.8	1.7	4.6	0.8	9.6	3.6	6.2	2.3	0.0	0.0	14.4	0.0	10.3	0.4	0.1	2.0	0.4	0.2	0.0	0.0	0.9	3.6	4.9	86.7	0.0	2.1	0.3	0.0	0.0	4.3	2.9	2.9	0.7	0.0	13.3
HU90-023-045	60.9500	-66.1400	-845	5.09	0.0839	13.7	1.4	4.9	0.0	9.4	4.6	5.6	0.0	0.0	0.0	18.8	0.0	11.3	0.3	0.1	2.0	0.4	0.1	0.0	0.0	0.7	3.9	4.8	82.1	0.1	3.6	0.6	0.5	0.0	4.9	3.1	3.7	1.2	0.0	17.9
HU90-023-045	60.9500	-66.1400	-845	5.56	0.0932	8.9	0.4	4.8	0.0	8.1	2.4	3.9	0.6	0.0	0.1	26.1	1.1	15.3	0.2	0.2	1.2	0.7	0.1	0.0	0.0	0.8	4.3	4.1	83.3	0.6	3.6	0.6	0.1	0.0	4.1	3.0	4.0	0.6	0.0	16.7
HU90-023-045	60.9500	-66.1400	-845	6.06	0.0858	10.5	1.1	5.0	0.0	8.9	3.3	5.3	1.1	0.0	0.0	22.3	0.0	11.3	0.4	0.1	2.0	0.0	0.1	0.0	0.0	1.1	4.1	2.7	79.4	0.1	4.4	0.7	1.4	0.0	4.4	3.1	4.7	1.8	0.0	20.6
HU90-023-045	60.9500	-66.1400	-845	5.36	0.0890	10.5	0.4	6.3	1.2	5.4	3.6	5.1	0.1	0.0	0.0	17.7	3.8	11.6	0.4	0.2	1.7	0.0	0.0	0.3	0.0	0.2	3.3	1.8	73.5	0.0	3.2	0.4	3.0	0.0	4.7	4.1	7.1	4.0	0.0	26.5
HU90-023-045	60.9500	-66.1400	-845	5.52	0.0934	8.8	0.2	6.3	0.0	5.0	2.5	5.3	0.5	0.0	0.0	27.4	2.7	13.8	0.2	0.2	1.2	0.2	0.0	0.1	0.0	0.2	3.7	2.1	80.5	0.0	2.2	0.1	1.1	0.0	3.2	4.0	7.0	1.9	0.0	19.5
HU90-023-045	60.9500	-66.1400	-845	5.92	0.0844	7.5	0.6	5.9	0.0	3.7	3.5	5.8	1.9	0.0	0.0	24.7	0.2	11.2	0.4	0.1	2.0	0.0	0.1	0.2	0.0	0.9	4.3	3.0	75.8	0.4	3.7	0.6	2.8	0.0	4.4	3.7	6.7	1.9	0.1	24.2
HU90-023-045	60.9500	-66.1400	-845	6.08	0.0985	9.7	0.4	5.9	0.0	8.4	3.2	5.4	1.0	0.0	0.0	21.4	0.4	10.4	0.5	0.0	1.8	0.9	0.3	0.1	0.0	0.3	3.8	2.9	76.8	0.0	2.3	0.3	3.4	0.0	5.0	4.6	6.3	1.2	0.0	23.2
HU90-023-045	60.9500	-66.1400	-845	6.18	0.0948	9.1	0.0	6.0	0.0	8.6	4.1	5.8	0.6	0.0	0.0	20.3	0.0	9.7	0.6	0.1	2.3	0.6	0.2	0.0	0.0	0.8	3.9	2.9	75.7	0.1	3.0	0.2	3.4	0.0	5.1	4.6	6.3	1.5	0.0	24.3
HU90-023-045	60.9500	-66.1400	-845	6.43	0.0962	9.9	1.1	5.8	0.0	7.7	3.0	6.7	0.6	0.0	0.0	20.8	0.0	11.2	0.3	0.3	2.1	0.1	0.2	0.0	0.0	0.9	3.6	3.4	77.5	0.0	3.4	0.0	3.3	0.0	4.2	4.4	6.0	1.2	0.0	22.5
HU90-023-045	60.9500	-66.1400	-845	6.55	0.0934	9.7	0.7	5.8	0.0	7.2	4.0	5.3	0.8	0.0	0.0	18.3	0.0	10.5	0.4	0.4	1.8	0.8	0.2	0.0	0.0	2.4	4.4	4.1	76.9	0.0	3.4	0.0	3.0	0.0	3.9	4.5	6.5	1.8	0.0	23.1
HU90-023-045	60.9500	-66.1400	-845	6.63	0.1092	7.4	0.0	6.0	0.0	7.1	2.5	5.3	1.0	0.0	0.0	22.5	0.0	10.9	0.6	1.0	1.8	0.0	0.1	0.0	0.1	2.1	4.8	3.8	77.0	0.0	3.3	0.0	3.5	0.0	3.4	4.5	6.8	1.5	0.0	23.0
HU90-023-091	63.0460	-81.9880	-212	1.00	0.0978	8.5	0.0	5.8	0.0	6.4	3.2	3.6	0.0	0.0	0.0	27.1	1.3	14.5	0.7	0.1	1.7	0.6	0.0	0.0	0.0	1.8	4.6	2.8	82.5	0.2	2.1	0.1	2.7	0.0	2.5	3.4	5.3	0.5	0.7	17.5
HU90-023-091	63.0460	-81.9880	-212	1.23	0.0959	9.5	0.0	6.5	1.8	4.8	3.4	3.1	0.0	0.0	0.0	14.1	3.0	13.3	0.6	0.2	1.2	0.1	0.0	0.0	0.1	1.7	3.3	1.4	67.7	0.0	5.3	0.6	7.1	0.0	5.0	3.0	6.9	4.4	0.0	32.3
HU90-023-091	63.0460	-81.9880	-212	1.30	0.0791	9.1	0.3	6.6	1.8	5.5	3.5	2.7	0.0	0.0	0.1	12.9	0.1	19.1	0.2	0.3	0.6	0.2	0.0	0.0	0.2	0.0	3.1	3.0	69.3	0.0	3.9	0.1	6.5	0.0	6.5	2.4	7.0	4.2	0.0	30.7
HU90-023-091	63.0460	-81.9880	-212	1.38	0.0904	10.2	0.4	7.5	2.0	4.1	4.2	2.4	0.0	0.0	0.0	11.8	2.4	17.6	0.3	0.0	0.7	0.5	0.1	0.0	0.0	1.0	2.9	2.2	70.3	0.0	3.2	0.0	5.1	0.0	6.0	2.7	7.5	5.2	0.0	29.7
HU90-023-091	63.0460	-81.9880	-212	1.45	0.0814	9.4	0.8	7.8	0.7	4.8	3.8	3.1	0.0	0.0	0.0	13.4	0.0	19.7	0.4	0.2	0.5	0.1	0.1	0.0	0.1	0.9	3.1	2.4	71.4	0.0	4.2	0.0	4.5	0.0	5.5	2.5	7.8	4.0	0.0	28.6
HU90-023-091	63.0460	-81.9880	-212	1.80	0.1020	7.0	0.0	6.6	0.0	1.8	1.8	4.7	0.0	1.4	0.0	40.9	0.2	14.9	0.2	0.1	1.3	1.0	0.0	0.0	0.0	0.4	3.1	2.2	87.5	0.0	2.1	0.1	0.1	0.1	1.3	2.0	6.5	0.2	0.2	12.5
HU90-023-099	63.0660	-74.5660	-386	0.69	0.0917	6.3	0.0	4.3	0.0	5.0	1.9	2.6	0.4	0.0	0.0	33.2	4.5	18.2	0.3	0.2	0.7	0.7	0.1	0.0	0.0	0.4	4.3	2.4	85.6	0.8	2.7	0.6	0.4	0.3	2.5	2.7	4.0	0.0	0.4	14.4
HU90-023-099	63.0660	-74.5660	-386	0.96	0.0893	7.2	0.1	4.6	0.0	6.1	2.3	3.3	0.0	0.0	0.2	31.7	1.5	15.9	0.4	0.1	0.9	0.3	0.1	0.0	0.0	1.2	4.1	1.6	81.6	1.3	3.9	0.9	1.3	0.0	3.3	2.6	4.5	0.6	0.0	18.4
HU90-023-099	63.0660	-74.5660	-386	1.34	0.0958	11.7	0.5	5.9	0.2	6.5	2.5	5.0	1.9	0.0	0.0	24.7	0.4	13.7	0.5	0.0	1.3	0.4	0.1	0.0	0.0	0.8	4.2	1.5	81.8	0.7	3.2	0.6	1.3	0.0	5.2	1.9	5.2	0.1	0.0	18.2
HU90-023-099	63.0660	-74.5660	-386	1.98	0.0827	7.0	0.1	5.6	0.0	3.8	3.0	4.7	1.2	0.0	0.0	26.9	0.0	14.0	0.3	0.2	0.9	0.0	0.0	0.0	0.0	1.2	4.5	1.6	75.2	1.9	5.0	1.2	1.9	0.0	5.4	2.1	6.1	1.2	0.0	24.8
HU90-023-099	63.0660	-74.5660	-386	2.33	0.0897	11.2	1.2	5.3	0.0	4.4	2.7	5.6	1.9	0.0	0.0	24.8	0.0	15.1	0.2	0.2	1.2	0.4	0.1	0.0	0.0	0.7	4.3	2.8	82.0	0.5	3.2	0.7	0.5	0.1	5.1	1.9	5.5	0.5	0.0	18.0
HU90-023-099	63.0660	-74.5660	-386	0.69	0.0876	8.1	0.0	5.3	0.0	6.1	1.8	4.1	0.6	0.0	0.0	30.8	0.0	13.5	0.5	0.0	0.7	0.0	0.1	0.0	0.0	1.0	4.7	1.9	79.2	2.3	3.5	1.0	0.5	0.0	4.5	1.9	5.5	1.5	0.0	20.8
HU90-023-101	63.0490	-74.3040	-389	0.69	0.0891	12.2	1.3	5.2	0.4	6.4	5.0	7.2	2.7	0.0	0.0	14.8	0.0	13.2	0.2	0.5	2.6	0.2	0.3	0.0	0.0	0.6	4.7	3.7	81.2	0.0	3.5	0.7	0.0	0.0	5.9	2.2	5.6	0.9	0.0	18.8
HU90-023-101	63.0490	-74.3040	-389	1.34	0.0902	8.0	0.3	5.5	0.0	5.2	3.6	5.6	0.8	0.0	0.0	22.5	0.0	14.4	0.1	0.3	2.0	0.4	0.2	0.0	0.0	0.9	5.1	3.2	78.0	0.2	5.2	0.9	0.1	0.0	6.0	2.6	6.5	0.5	0.0	22.0
HU90-023-101	63.0490	-74.3040	-389	1.62	0.0822	11.3	1.3	5.2	0.3	5.5	5.1	6.8	1.8	0.0	0.0	20.7	0.0	11.2	0.2	0.3	1.9	0.6	0.2	0.0	0.0	0.6	4.7	2.9	80.5	0.0	4.4	0.7	0.0	0.0	5.7	2.4	5.9	0.5	0.0	19.5
HU90-023-101	63.0490	-74.3040	-389	2.63	0.0854	8.4	1.1	5.3	0.0	5.0	3.1	5.4	1.0	0.0	0.0	25.2	0.6	14.2	0.1	0.1	1.3	0.3	0.2	0.0	0.0	0.8	4.7	3.1	79.9	0.2	4.5	0.6	0.0	0.0	5.6	2.4	6.1	0.6	0.0	20.1
HU90-023-101	63.0490	-74.3040	-389	3.39	0.0869	9.9	0.7	5.4	0.0	4.1	3.0	6.1	1.2	0.0	0.0	26.8	1.2	13.6	0.5	0.3	1.7	0.1	0.1	0.0	0.0	1.3	3.9	1.9	81.9	0.3	4.1	1.1	0.0	0.0	3.7	2.0	5.6	1.3	0.0	18.1
HU90-023-101	63.0490	-74.3040	-389	0.91	0.0914	11.5	0.6	6.5	0.0	3.0	3.4	7.6	1.2	0.0	0.0	21.2	0.0	13.0	0.3	0.5	1.8	0.2	0.0	0.2	0.1	0.6	3.3	4.5	79.6	0.0	3.5	0.1	2.0	0.0	3.7	2.2	6.5	1.6	0.8	20.4
HU90-023-101	63.0490	-74.3040	-389	0.97	0.0831	15.8	1.3	5.9	1.7	0.0	4.2	8.0	2.4	0.0	0.0	19.8	2.1	16.2	0.2	0.2	1.4	0.0	0.1	0.0	0.1	0.0	1.8	1.5	82.6	0.1	2.1	0.6	2.2	0.3	3.7	1.6	5.2	1.6	0.0	17.4
HU90-023-101	63.0490	-74.3040	-389	2.17	0.0816	8.3	0.8	6.6	0.6	3.0	3.8	4.0	0.6	0.0	0.3	15.0	0.0	20.0	0.3	0.4	0.7	1.1	0.2	0.0	0.0	1.7	2.5	3.4	73.3	0.0	4.2	0.6	3.3	0.0	5.9	2.1	6.3	4.1	0.0	26.7
HU90-023-101	63.0490	-74.3040	-389	2.18	0.0843	8.7	0.4	6.5	1.4	3.7	3.9	3.4	0.0	0.0	0.0	14.7	0.0	20.2	0.3	0.3	0.5	0.1	0.1	0.0	0.0	1.9	2.6	3.4	72.0	0.0	4.7	0.5	3.9	0.0	5.7	2.0	6.5	4.6	0.0	28.0
HU90-023-101	63.0490	-74.3040	-389	2.25	0.0903	11.2	0.3	6.3	0.0	4.1	3.6	4.8	1.2	0.0	0.0	22.9	0.1	14.9	0.5	0.1	1.2	0.4	0.1	0.0	0.1	1.8	2.6	3.0	79.3	0.0	4.0	0.2	2.1	0.0	3.9	2.0	6.1	2.4	0.0	20.7