Murdmaa, Ivar O; Bazilevskaya, Elena S; Gordeev, Viacheslav V; Emelyanov, Emelyan M; Kuz'mina, Tatyana G; Turanskaya, Natalya V (1979): (Table 13) Chemical composition of sedimentary and volcano-sedimentary rocks from different formations drilled in holes of DSDP Legs 43 and 44 [dataset]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.733290, In supplement to: Murdmaa, Ivar O; Bazilevskaya, Elena S; Gordeev, Viacheslav V; Emelyanov, Emelyan M; Kazakova, Vera P; Kuz'mina, Tatyana G; Mukhina, Valentina V; Rudakova, Alevtina N; Turanskaya, Natalya V (1979): Geological Formations of the Southwest Atlantic Ocean. Bezrukov, P.L. (Ed.), Nauka Publ. (Moscow): in Russian, 207 pp.
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Related to:
Murdmaa, Ivar O; Bazilevskaya, Elena S; Gordeev, Viacheslav V; Emelyanov, Emelyan M; Kuz'mina, Tatyana G; Turanskaya, Natalya V (1979): Geochemical characteristics of the sedimentary formations. In: Bezrukov, P.L. (Ed.), Geological Formations of the Southwest Atlantic Ocean; Nauka Publ. (Moscow): in Russian, 96-147
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 31.957867 * Median Longitude: -66.640683 * South-bound Latitude: 28.226800 * West-bound Longitude: -75.616700 * North-bound Latitude: 37.369500 * East-bound Longitude: -56.537500
Date/Time Start: 1975-07-05T00:00:00 * Date/Time End: 1975-09-02T00:00:00
Minimum Elevation: -5526.0 m * Maximum Elevation: -4782.0 m
Event(s):
43-382 * Latitude: 34.417300 * Longitude: -56.537500 * Date/Time: 1975-07-05T00:00:00 * Elevation: -5526.0 m * Penetration: 520.5 m * Recovery: 162 m * Location: North Atlantic/SEAMOUNT * Campaign: Leg43 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 25 cores; 233.3 m cored; 0 m drilled; 69.4 % recovery
43-385 * Latitude: 37.369500 * Longitude: -60.157500 * Date/Time: 1975-07-18T00:00:00 * Elevation: -4936.0 m * Penetration: 392.9 m * Recovery: 64 m * Location: North Atlantic/SEAMOUNT * Campaign: Leg43 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 218.2 m cored; 9.5 m drilled; 29.3 % recovery
43-386 * Latitude: 31.186800 * Longitude: -64.249000 * Date/Time: 1975-07-24T00:00:00 * Elevation: -4782.0 m * Penetration: 973.8 m * Recovery: 434.3 m * Location: North Atlantic/CONT RISE * Campaign: Leg43 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 65 cores; 617.4 m cored; 9.5 m drilled; 70.3 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | Sample code/label | Sample label | Murdmaa, Ivar O | DSDP/ODP/IODP sample designation | ||
6 | Formation | Formation | Murdmaa, Ivar O | |||
7 | Comment | Comment | Murdmaa, Ivar O | |||
8 | Silicon dioxide | SiO2 | % | Murdmaa, Ivar O | Wet chemistry | |
9 | Titanium dioxide | TiO2 | % | Murdmaa, Ivar O | Wet chemistry | |
10 | Aluminium oxide | Al2O3 | % | Murdmaa, Ivar O | Wet chemistry | |
11 | Iron oxide, Fe2O3 | Fe2O3 | % | Murdmaa, Ivar O | Wet chemistry | total Fe expressed as Fe2O3 |
12 | Manganese oxide | MnO | % | Murdmaa, Ivar O | Wet chemistry | |
13 | Magnesium oxide | MgO | % | Murdmaa, Ivar O | Wet chemistry | |
14 | Calcium oxide | CaO | % | Murdmaa, Ivar O | Wet chemistry | |
15 | Potassium oxide | K2O | % | Murdmaa, Ivar O | Wet chemistry | |
16 | Sodium oxide | Na2O | % | Murdmaa, Ivar O | Wet chemistry | |
17 | Phosphorus pentoxide | P2O5 | % | Murdmaa, Ivar O | Wet chemistry | |
18 | Loss on ignition | LOI | % | Murdmaa, Ivar O | Calculated from weight loss after ignition at 450 °C | |
19 | Silicon/Aluminium ratio | Si/Al | Murdmaa, Ivar O | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1269 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Formation | 7 Comment | 8 SiO2 [%] | 9 TiO2 [%] | 10 Al2O3 [%] | 11 Fe2O3 [%] | 12 MnO [%] | 13 MgO [%] | 14 CaO [%] | 15 K2O [%] | 16 Na2O [%] | 17 P2O5 [%] | 18 LOI [%] | 19 Si/Al |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-1-5,110-112 | terrigenous turbidite formation | 45.80 | 0.57 | 12.90 | 4.64 | 0.08 | 5.85 | 9.77 | 2.96 | 14.4 | 3.1 | |||
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-3-1,126-128 | terrigenous turbidite formation | 50.00 | 0.68 | 15.20 | 6.58 | 0.07 | 3.88 | 6.29 | 3.32 | 12.2 | 2.9 | |||
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-7-2,81-83 | hemipelagic clayey formation | 57.80 | 0.84 | 17.00 | 7.43 | 0.05 | 2.49 | 0.48 | 2.93 | 1.47 | 0.12 | 9.4 | 3.0 | |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-15-6,60-62 | formation of speckled clays | 55.10 | 0.65 | 15.69 | 5.97 | 1.38 | 3.87 | 0.67 | 3.23 | 1.56 | 0.35 | 11.8 | 3.1 | |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-6,45-48 | volcanoclastic formation of the New England Seamount Chain | 36.20 | 6.17 | 12.40 | 17.40 | 0.40 | 1.90 | 3.03 | 2.63 | 2.79 | 0.04 | 15.7 | 2.6 | |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-20-2,36-38 | volcanoclastic formation of the New England Seamount Chain | 39.50 | 4.60 | 14.90 | 11.80 | 0.24 | 4.28 | 3.09 | 3.95 | 3.26 | 0.21 | 13.8 | 2.3 | |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-20-5,55-57 | volcanoclastic formation of the New England Seamount Chain | 39.10 | 2.96 | 12.10 | 12.70 | 0.11 | 9.12 | 4.51 | 3.05 | 2.63 | 1.15 | 12.3 | 2.9 | |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-21-3,82-84 | volcanoclastic formation of the New England Seamount Chain | 41.70 | 4.83 | 14.40 | 10.60 | 0.15 | 5.20 | 2.40 | 5.23 | 5.56 | 0.66 | 9.7 | 2.6 | |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-25-2,49-51 | volcanoclastic formation of the New England Seamount Chain | 32.40 | 4.16 | 11.10 | 12.30 | 0.20 | 2.70 | 12.20 | 3.72 | 1.31 | 0.18 | 19.5 | 2.6 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-3-2,130-132 | hemipelagic clayey formation | 57.00 | 0.84 | 16.10 | 6.40 | 0.06 | 3.22 | 0.31 | 2.18 | 2.40 | 0.09 | 11.8 | 3.1 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-8-5,130-132 | formation of speckled clays | 57.10 | 0.58 | 15.20 | 5.75 | 0.09 | 2.94 | 0.49 | 3.02 | 2.07 | 0.19 | 11.4 | 3.3 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-10-1,138-140 | formation of speckled clays | 69.60 | 0.57 | 10.00 | 4.26 | 0.15 | 1.92 | 0.47 | 1.70 | 9.6 | 6.1 | |||
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-11-2,24-26 | formation of speckled clays | 53.00 | 0.61 | 14.50 | 6.72 | 0.75 | 3.18 | 0.92 | 3.32 | 13.8 | 3.2 | |||
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-13-3,109-113 | formation of speckled clays | 33.70 | 0.48 | 12.70 | 7.15 | 0.54 | 2.23 | 18.60 | 1.48 | 1.90 | 1.14 | 21.0 | 2.3 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-14-1,6 6-7 0 | formation of speckled clays | 53.30 | 0.87 | 19.30 | 8.18 | 0.40 | 2.39 | 0.33 | 2.98 | 1.05 | 0.15 | 11.1 | 2.4 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-14-2,6-8 | formation of speckled clays | 52.90 | 0.79 | 18.60 | 7.02 | 0.22 | 2.85 | 0.41 | 3.30 | 1.70 | 3.13 | 12.2 | 2.5 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-15-1,53-55 | formation of speckled clays | 51.10 | 1.00 | 19.40 | 9.87 | 0.15 | 2.29 | 0.38 | 3.11 | 1.23 | 0.15 | 11.1 | 2.3 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,122-123 | volcanoclastic formation of the New England Seamount Chain | 50.20 | 2.69 | 15.60 | 10.40 | 0.01 | 2.68 | 1.41 | 4.97 | 10.6 | 2.8 | |||
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,123-124 | volcanoclastic formation of the New England Seamount Chain | 48.20 | 2.15 | 15.76 | 11.78 | 0.68 | 3.19 | 1.17 | 4.87 | 11.4 | 2.7 | |||
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,8-10 | volcanoclastic formation of the New England Seamount Chain | 48.70 | 3.46 | 14.80 | 11.20 | 0.29 | 3.83 | 1.00 | 3.64 | 1.52 | 0.50 | 11.4 | 2.9 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-3,77-80 | volcanoclastic formation of the New England Seamount Chain | 48.40 | 1.08 | 19.10 | 8.78 | 1.66 | 2.45 | 0.74 | 4.65 | 1.06 | 0.45 | 10.8 | 2.2 | |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-23-1,128-134 | volcanoclastic formation of the New England Seamount Chain | 38.80 | 3.86 | 11.50 | 15.20 | 0.15 | 2.98 | 10.50 | 5.90 | 1.88 | 8.7 | 3.0 | ||
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-23-3,142-150 | volcanoclastic formation of the New England Seamount Chain | 18.40 | 4.56 | 6.90 | 15.60 | 0.17 | 4.15 | 18.30 | 2.00 | 4.15 | 0.41 | 25.3 | 2.4 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-2,111-115 | basalt-greywacke formation of the Bermuda massife | 51.20 | 1.84 | 14.80 | 8.28 | 0.10 | 3.66 | 1.99 | 2.83 | 12.1 | 3.1 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-6-4,128-133 | basalt-greywacke formation of the Bermuda massife | 36.00 | 4.10 | 10.40 | 13.80 | 0.34 | 9.77 | 12.60 | 1.38 | 0.95 | 0.44 | 9.1 | 3.1 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-8-1,147-150 | basalt-greywacke formation of the Bermuda massife | 33.40 | 3.84 | 11.30 | 10.50 | 3.00 | 7.05 | 11.00 | 2.19 | 0.90 | 0.44 | 16.7 | 2.6 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-8-6,134-137 | basalt-greywacke formation of the Bermuda massife | 32.80 | 4.62 | 9.70 | 12.30 | 4.06 | 9.48 | 14.80 | 1.34 | 1.51 | 0.34 | 9.6 | 3.0 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-9-3,127-130 | basalt-greywacke formation of the Bermuda massife | 34.30 | 4.37 | 10.40 | 12.60 | 0.27 | 9.38 | 14.30 | 1.99 | 1.53 | 0.55 | 10.4 | 2.9 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-13-3,127-133 | basalt-greywacke formation of the Bermuda massife | 32.20 | 2.03 | 5.75 | 6.25 | 0.25 | 3.50 | 23.20 | 1.99 | 1.21 | 0.43 | 23.0 | 4.9 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-14-4,19-21 | carbonaceous-siliceous-clayey (turbidite) formation | 54.20 | 0.59 | 12.50 | 7.76 | 0.05 | 3.35 | 2.17 | 2.19 | 1.68 | 0.19 | 14.8 | 3.8 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-28-2,123-125 | carbonaceous-siliceous-clayey (turbidite) formation | 57.20 | 0.39 | 9.52 | 4.71 | 0.09 | 2.50 | 7.91 | 1.29 | 1.38 | 0.05 | 15.0 | 5.3 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-28-4,108-110 | carbonaceous-siliceous-clayey (turbidite) formation | 65.50 | 0.34 | 8.10 | 3.18 | 0.03 | 2.20 | 5.75 | 1.22 | 0.76 | 0.14 | 12.6 | 7.1 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-30-2,89-91 | carbonaceous-siliceous-clayey (turbidite) formation | 83.50 | 0.23 | 5.70 | 1.16 | 0.01 | 0.49 | 0.64 | 0.89 | 1.15 | 5.8 | 12.9 | ||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-30-6,59-61 | carbonaceous-siliceous-clayey (turbidite) formation | 51.70 | 0.21 | 7.57 | 1.91 | 0.14 | 1.76 | 15.10 | 1.04 | 1.68 | 0.05 | 18.9 | 6.0 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-31-1,46-49 | carbonaceous-siliceous-clayey (turbidite) formation | 46.70 | 0.34 | 10.60 | 4.25 | 0.10 | 2.35 | 15.50 | 1.56 | 0.55 | 0.17 | 18.2 | 3.9 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-34-6,29-31 | carbonaceous-siliceous-clayey (turbidite) formation | 58.80 | 0.60 | 14.30 | 6.77 | 0.33 | 2.38 | 1.35 | 2.36 | 11.7 | 3.6 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-36-5,74-76 | formation of speckled clays | 52.80 | 0.87 | 19.10 | 7.46 | 0.72 | 2.33 | 0.74 | 3.33 | 0.90 | 0.23 | 11.4 | 2.4 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-36-5,94-98 | formation of speckled clays | 52.70 | 0.83 | 19.40 | 7.39 | 0.66 | 3.42 | 0.68 | 2.09 | 0.20 | 0.17 | 11.9 | 2.4 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-37-3,15-17 | formation of speckled clays | 71.10 | 0.50 | 9.67 | 5.04 | 0.03 | 1.86 | 0.51 | 1.92 | 7.0 | 6.5 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-37-3,8-9 | formation of speckled clays | 64.90 | 0.45 | 10.43 | 5.17 | 0.03 | 1.81 | 0.81 | 1.69 | 13.1 | 5.5 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-38-1,31-32 | formation of speckled clays | 69.60 | 0.39 | 8.93 | 5.08 | 1.46 | 1.33 | 0.58 | 1.22 | 2.54 | 8.9 | 6.9 | ||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-38-3,90-91 | formation of speckled clays | 68.30 | 0.50 | 10.50 | 5.95 | 0.27 | 1.48 | 0.82 | 1.46 | 1.37 | 0.22 | 9.2 | 5.7 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-39-1,129-131 | formation of speckled clays | 63.80 | 0.56 | 13.20 | 7.00 | 0.11 | 1.33 | 0.81 | 1.82 | 1.20 | 0.22 | 9.6 | 4.3 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-39-1,144-145 | formation of speckled clays | 60.80 | 0.53 | 13.40 | 7.23 | 1.05 | 2.08 | 0.74 | 1.68 | 1.49 | 0.26 | 10.4 | 4.0 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-40-2,0-1 | formation of speckled clays | 71.80 | 0.38 | 9.54 | 3.34 | 0.23 | 1.32 | 0.64 | 1.41 | 1.66 | 0.21 | 8.9 | 6.6 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-40-2,3-4 | formation of speckled clays | 63.40 | 0.51 | 12.70 | 8.55 | 0.52 | 1.38 | 0.68 | 1.72 | 0.01 | 0.21 | 10.4 | 4.4 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-41-4,68-70 | formation of speckled clays | 64.30 | 0.45 | 11.43 | 8.57 | 0.06 | 1.47 | 0.71 | 1.69 | 9.3 | 5.0 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-42-2,105-107 | formation of black clays | 83.60 | 0.09 | 3.17 | 1.22 | 0.54 | 1.12 | 1.86 | 0.27 | 0.15 | 7.1 | 23.3 | ||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-44-3,20-21 | formation of black clays | 72.50 | 0.26 | 8.22 | 3.63 | 0.40 | 1.71 | 0.62 | 1.22 | 9.9 | 7.8 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-44-3,23.5-25 | formation of black clays | 61.80 | 0.27 | 7.40 | 3.07 | 0.21 | 1.74 | 1.30 | 1.01 | 22.1 | 7.4 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-44-3,23-25 | formation of black clays | 83.20 | 0.07 | 3.06 | 1.35 | 0.16 | 0.33 | 3.37 | 0.29 | 7.7 | 24.0 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-48-3,123-124 | formation of black clays | 26.30 | 0.08 | 4.70 | 1.17 | 0.86 | 0.78 | 33.00 | 0.11 | 0.10 | 32.4 | 4.9 | ||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-49-3,90-93 | formation of black clays | 63.40 | 0.34 | 8.68 | 4.52 | 1.94 | 2.26 | 5.09 | 1.25 | 0.92 | 0.06 | 11.4 | 6.5 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-60-5,140-141 | formation of black clays | 64.50 | 0.41 | 9.50 | 5.05 | 0.26 | 2.48 | 1.86 | 1.90 | 1.02 | 0.18 | 12.4 | 6.0 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-63-4,82-84 | formation of black clays | 57.10 | 0.38 | 8.44 | 13.55 | 0.04 | 1.43 | 0.43 | 3.28 | 15.6 | 6.0 | |||
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-64-3,22-23 | formation of black clays | 71.30 | 0.36 | 7.02 | 7.03 | 0.06 | 2.35 | 0.37 | 2.69 | 0.87 | 0.10 | 5.3 | 9.0 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-64-3,24-25 | formation of black clays | 70.70 | 0.33 | 7.32 | 10.20 | 0.05 | 2.28 | 0.30 | 2.53 | 0.79 | 0.17 | 5.4 | 8.5 | |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-65-3,99-101 | formation of black clays | 51.90 | 0.39 | 7.94 | 16.04 | 0.03 | 3.17 | 0.73 | 2.24 | 16.9 | 5.8 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-7-3,80-83 | carbonaceous-siliceous-clayey (turbidite) formation | 64.80 | 0.45 | 10.27 | 4.73 | 0.72 | 2.55 | 0.74 | 1.35 | 12.6 | 5.6 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-10-5,89-91 | carbonaceous-siliceous-clayey (turbidite) formation | 69.50 | 0.20 | 5.09 | 1.81 | 0.34 | 0.57 | 6.00 | 0.61 | 13.6 | 12.1 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-18-1,81-83 | carbonaceous-siliceous-clayey (turbidite) formation | 53.30 | 0.16 | 5.59 | 1.59 | 0.19 | 2.67 | 15.86 | 0.67 | 19.9 | 8.4 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-18-1,81-83 | carbonaceous-siliceous-clayey (turbidite) formation | 80.70 | 0.24 | 6.58 | 1.97 | 0.03 | 0.95 | 0.65 | 0.64 | 7.0 | 10.8 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-18-1,84-86 | carbonaceous-siliceous-clayey (turbidite) formation | 80.90 | 0.19 | 5.88 | 1.71 | 0.02 | 0.65 | 0.48 | 0.55 | 6.9 | 12.2 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-19-1,103-108 | carbonaceous-siliceous-clayey (turbidite) formation | 57.10 | 0.24 | 7.53 | 2.22 | 0.08 | 1.85 | 11.71 | 0.88 | 17.6 | 6.7 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-19-2,61-63 | carbonaceous-siliceous-clayey (turbidite) formation | 78.30 | 0.15 | 3.10 | 1.06 | 0.04 | 0.60 | 8.12 | 0.36 | 8.2 | 22.3 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-19-3,20-22 | carbonaceous-siliceous-clayey (turbidite) formation | 72.70 | 0.33 | 8.42 | 3.73 | 0.29 | 1.41 | 0.71 | 1.09 | 9.5 | 7.6 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-25-3,144-146 | carbonaceous-siliceous-clayey (turbidite) formation | 80.70 | 0.23 | 6.14 | 2.01 | 0.02 | 1.84 | 1.10 | 0.83 | 0.55 | 0.21 | 6.6 | 11.6 | |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-26-2,0-2 | carbonaceous-siliceous-clayey (turbidite) formation | 66.80 | 0.77 | 11.60 | 5.36 | 0.04 | 2.62 | 0.44 | 1.87 | 1.52 | 0.18 | 8.9 | 5.1 | |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-29-2,12-15 | formation of speckled clays | 53.60 | 0.94 | 19.30 | 8.65 | 0.11 | 2.37 | 0.46 | 3.55 | 1.83 | 0.20 | 9.8 | 2.5 | |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-34-4,117-119 | formation of black clays | 71.30 | 0.35 | 8.78 | 3.97 | 0.02 | 1.22 | 1.19 | 1.10 | 10.0 | 7.2 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-34-4,96-98 | formation of black clays | 74.80 | 0.36 | 9.03 | 3.59 | 0.02 | 1.09 | 0.58 | 1.12 | 6.4 | 7.3 | |||
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-37-2,101-103 | formation of black clays | 72.00 | 0.44 | 9.70 | 3.64 | 0.02 | 4.60 | 0.47 | 1.65 | 1.17 | 0.23 | 6.3 | 6.6 | |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-42-1,72-75 | ancient carbonate formation (gray-colored sub-formation) | 19.20 | 0.15 | 4.50 | 2.75 | 0.03 | 2.95 | 4.40 | 1.41 | 0.42 | 0.28 | 33.7 | 3.8 | |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-42-1,72-75 | ancient carbonate formation (gray-colored sub-formation) | contents calculated on carbonate-free basis | 50.35 | 0.39 | 11.80 | 7.21 | 0.08 | 7.74 | 0.00 | 3.70 | 1.10 | 0.73 | 16.6 | |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-50-1,35-38 | ancient carbonate formation (gray-colored sub-formation) | 48.70 | 1.03 | 15.70 | 7.48 | 0.06 | 9.80 | 10.10 | 0.09 | 1.25 | 0.13 | 4.8 | 2.7 | |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-17-4,139-142 | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | 46.40 | 0.32 | 9.24 | 2.97 | 0.05 | 3.21 | 14.69 | 1.02 | 19.9 | 4.4 | |||
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-17-4,139-142 | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | contents calculated on carbonate-free basis | 62.77 | 0.43 | 12.50 | 4.02 | 0.07 | 4.34 | 1.77 | 1.38 | 12.7 | |||
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-1,63-67 | formation of speckled clays | 55.80 | 0.97 | 18.12 | 8.00 | 0.12 | 2.15 | 0.47 | 2.69 | 10.3 | 2.7 | |||
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-1,75-79 | formation of speckled clays | 54.00 | 0.93 | 17.95 | 8.48 | 0.79 | 1.79 | 0.60 | 2.69 | 10.2 | 2.7 | |||
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-2,88-89 | formation of speckled clays | 49.30 | 0.86 | 16.45 | 16.00 | 0.12 | 2.16 | 0.52 | 2.80 | 11.6 | 2.6 | |||
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-3,93-96 | formation of speckled clays | 54.40 | 0.84 | 16.46 | 10.21 | 0.05 | 1.49 | 0.42 | 2.86 | 12.0 | 2.9 | |||
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-5,8-10 | formation of speckled clays | 52.70 | 0.91 | 18.46 | 7.11 | 0.04 | 2.94 | 0.54 | 2.53 | 11.6 | 2.5 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-2-2,6-10 | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | 21.10 | 0.06 | 4.00 | 1.62 | 0.02 | 2.23 | 35.93 | 0.02 | 35.5 | 4.7 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-2-2,6-10 | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | contents calculated on carbonate-free basis | 63.65 | 0.18 | 12.07 | 4.89 | 0.06 | 6.73 | 0.00 | 0.06 | 12.4 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-4-1,107-110 | formation of speckled clays | 54.10 | 0.88 | 17.89 | 8.09 | 0.04 | 2.74 | 0.52 | 2.47 | 12.3 | 2.7 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-5-1,72-75 | formation of speckled clays | 53.10 | 0.90 | 17.19 | 10.49 | 0.10 | 2.43 | 0.65 | 2.84 | 9.6 | 2.7 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-6-1,56-61 | formation of speckled clays | 56.20 | 0.88 | 17.27 | 10.33 | 0.04 | 1.68 | 0.52 | 2.83 | 8.6 | 2.9 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-10-1,72-75 | formation of black clays | 56.00 | 0.80 | 15.98 | 7.94 | 0.04 | 2.83 | 0.60 | 2.60 | 12.2 | 3.1 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-10-2,108-111 | formation of black clays | 54.00 | 0.76 | 14.85 | 11.34 | 0.10 | 2.92 | 0.47 | 3.18 | 10.0 | 3.2 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-15-3,83-86 | ancient carbonate formation (gray-colored sub-formation) | 45.90 | 0.53 | 11.69 | 5.16 | 0.03 | 3.39 | 9.67 | 2.62 | 17.4 | 3.5 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-15-3,83-86 | ancient carbonate formation (gray-colored sub-formation) | contents calculated on carbonate-free basis | 58.30 | 0.67 | 14.85 | 6.55 | 0.04 | 4.31 | 0.00 | 3.33 | 11.9 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-20-2,54-57 | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | 60.30 | 0.58 | 12.69 | 6.17 | 0.03 | 3.48 | 0.77 | 1.69 | 13.1 | 4.2 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-28-2,106-110 | ancient carbonate formation (gray-colored sub-formation) | 46.60 | 0.58 | 11.45 | 5.94 | 0.02 | 2.99 | 11.04 | 1.93 | 16.7 | 3.6 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-28-2,106-110 | ancient carbonate formation (gray-colored sub-formation) | contents calculated on carbonate-free basis | 59.11 | 0.74 | 14.52 | 7.53 | 0.02 | 3.79 | 0.91 | 2.45 | 10.9 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-49-2,81-83 | ancient carbonate formation (red-colored sub-formation) | 41.80 | 0.32 | 8.94 | 4.64 | 0.05 | 3.19 | 16.74 | 1.70 | 20.3 | 4.1 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-49-2,81-83 | ancient carbonate formation (red-colored sub-formation) | contents calculated on carbonate-free basis | 60.75 | 0.46 | 12.99 | 6.74 | 0.07 | 4.63 | 0.81 | 2.47 | 11.0 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-52-4,13-15 | ancient carbonate formation (red-colored sub-formation) | 41.20 | 0.44 | 10.37 | 7.06 | 0.06 | 3.45 | 13.33 | 2.29 | 19.2 | 3.5 | |||
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-52-4,13-15 | ancient carbonate formation (red-colored sub-formation) | contents calculated on carbonate-free basis | 56.03 | 0.60 | 14.10 | 9.60 | 0.07 | 4.69 | 0.00 | 3.11 | 11.8 |