Murdmaa, Ivar O; Bazilevskaya, Elena S; Gordeev, Viacheslav V; Emelyanov, Emelyan M; Kuz'mina, Tatyana G; Turanskaya, Natalya V (1979): (Table 16) Aluminum contents and element/aluminium ratios in sedimentary rocks of 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.733318, 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):
Archive of Ocean Data (ARCOD)
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 31.950444 * Median Longitude: -69.051633 * South-bound Latitude: 28.226800 * West-bound Longitude: -76.112300 * 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: -2665.0 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 | Aluminium | Al | % | Murdmaa, Ivar O | Atomic absorption spectrometry (AAS) | |
8 | Iron/Aluminium ratio | Fe/Al | Murdmaa, Ivar O | Calculated | ||
9 | Manganese/Aluminium ratio | Mn/Al | Murdmaa, Ivar O | Calculated | ||
10 | Titanium/Aluminium ratio | Ti/Al | Murdmaa, Ivar O | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
845 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Formation | 7 Al [%] | 8 Fe/Al | 9 Mn/Al | 10 Ti/Al |
---|---|---|---|---|---|---|---|---|---|
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-1-4,113-115 | terrigenous turbidite formation | 5.1 | 0.3 | 6.01 | 0.049 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-1-5,110-112 | terrigenous turbidite formation | 7.0 | 0.6 | 0.01 | 0.064 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-3-1,126-128 | terrigenous turbidite formation | 8.2 | 0.6 | 0.01 | 0.056 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-7-2,81-83 | hemipelagic clayey formation | 10.2 | 0.5 | 0.01 | 0.049 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-11-1,96-98 | hemipelagic clayey formation | 9.4 | 0.6 | 0.01 | 0.049 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-15-4,147-150 | formation of speckled clays | 9.8 | 0.6 | 0.01 | 0.048 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-15-6,44-47 | formation of speckled clays | 9.3 | 0.5 | 0.02 | 0.027 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-15-6,44-47 | formation of speckled clays | 9.5 | 0.4 | 0.06 | 0.032 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-15-6,60-62 | formation of speckled clays | 9.3 | 0.4 | 0.08 | 0.027 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-1,0-3 | formation of speckled clays | 10.4 | 0.6 | 0.01 | 0.048 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-6,45-48 | volcanoclastic formation of the New England Seamount Chain | 8.3 | 1.2 | 0.03 | 0.172 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-6,123-126 | volcanoclastic formation of the New England Seamount Chain | 8.2 | 1.0 | 0.03 | 0.182 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-1,61-65 | volcanoclastic formation of the New England Seamount Chain | 8.6 | 0.8 | 0.03 | 0.133 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-2,4-9 | volcanoclastic formation of the New England Seamount Chain | 5.3 | 0.7 | 0.02 | 0.143 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-2,109-112 | volcanoclastic formation of the New England Seamount Chain | 6.5 | 0.9 | 0.02 | 0.167 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-4,9-12 | volcanoclastic formation of the New England Seamount Chain | 6.5 | 1.0 | 0.02 | 0.156 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-20-2,36-38 | volcanoclastic formation of the New England Seamount Chain | 9.2 | 0.9 | 0.02 | 0.123 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-20-5,55-57 | volcanoclastic formation of the New England Seamount Chain | 6.5 | 0.3 | 0.03 | 0.137 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-21-3,82-84 | volcanoclastic formation of the New England Seamount Chain | 8.5 | 0.9 | 0.03 | 0.147 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-22-2,86-89 | volcanoclastic formation of the New England Seamount Chain | 8.2 | 0.8 | 0.02 | 0.208 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-24-1,90-93 | volcanoclastic formation of the New England Seamount Chain | 6.4 | 1.0 | 0.03 | 0.169 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-25-2,49-51 | volcanoclastic formation of the New England Seamount Chain | 5.9 | 1.5 | 0.02 | 0.417 |
43-382 | 34.4173 | -56.5375 | -5526 | 43-382-25-CC, | volcanoclastic formation of the New England Seamount Chain | 4.4 | 1.1 | 0.02 | 0.143 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-3-2,130-132 | hemipelagic clayey formation | 9.4 | 0.5 | 0.01 | 0.043 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-8-5,130-132 | formation of speckled clays | 8.6 | 0.4 | 0.02 | 0.029 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-10-1,138-140 | formation of speckled clays | 5.4 | 0.4 | 0.02 | 0.037 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-11-2,24-26 | formation of speckled clays | 7.8 | 0.6 | 0.07 | 0.047 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-12-2,31-33 | formation of speckled clays | 6.4 | 0.6 | 0.03 | 0.055 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-13-3,109-112 | formation of speckled clays | 7.0 | 0.6 | 0.05 | 0.041 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-14-1,65-70 | formation of speckled clays | 10.5 | 0.5 | 0.03 | 0.036 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-14-2,6-8 | formation of speckled clays | 10.0 | 0.5 | 0.02 | 0.040 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-15-1,53-56 | formation of speckled clays | 10.9 | 0.6 | 0.02 | 0.035 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-15-1,100-101 | formation of speckled clays | 12.9 | 0.4 | 0.10 | 0.039 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-15-1,148-150 | formation of speckled clays | 10.9 | 0.5 | 0.11 | 0.035 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,8-10 | volcanoclastic formation of the New England Seamount Chain | 10.9 | 0.8 | 0.02 | 0.104 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,122-123 | volcanoclastic formation of the New England Seamount Chain | 8.4 | 0.8 | 0.01 | 0.192 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,123-124 | volcanoclastic formation of the New England Seamount Chain | 8.3 | 0.9 | 0.06 | 0.164 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-3,77-80 | volcanoclastic formation of the New England Seamount Chain | 4.5 | 1.4 | 0.22 | 0.095 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-20-2,40-50 | volcanoclastic formation of the New England Seamount Chain | 10.8 | 0.5 | 0.01 | 0.058 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-23-1,10 | volcanoclastic formation of the New England Seamount Chain | 6.1 | 1.8 | 0.02 | 0.385 |
43-385 | 37.3695 | -60.1575 | -4936 | 43-385-23-3,23 | volcanoclastic formation of the New England Seamount Chain | 3.7 | 2.9 | 0.05 | 0.714 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-2,111-115 | basalt-greywacke formation of the Bermuda massife | 7.9 | 0.8 | 0.01 | 0.135 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-6-4,128-133 | basalt-greywacke formation of the Bermuda massife | 5.5 | 1.6 | 0.04 | 0.333 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-8-1,147-150 | basalt-greywacke formation of the Bermuda massife | 6.0 | 1.2 | 0.02 | 0.286 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-8-6,134-137 | basalt-greywacke formation of the Bermuda massife | 5.1 | 1.8 | 0.61 | 0.455 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-9-3,127-130 | basalt-greywacke formation of the Bermuda massife | 5.5 | 1.6 | 0.04 | 0.500 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-13-3,127-133 | basalt-greywacke formation of the Bermuda massife | 3.0 | 1.5 | 0.06 | 0.400 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-14-4,19-21 | carbonate-siliceous-clayey (turbidite) formation | 6.6 | 0.8 | 0.01 | 0.053 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-28-2,123-125 | carbonate-siliceous-clayey (turbidite) formation | 5.2 | 0.6 | 0.01 | 0.044 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-28-4,108-110 | carbonate-siliceous-clayey (turbidite) formation | 4.3 | 0.5 | 0.01 | 0.047 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-30-2,89-91 | carbonate-siliceous-clayey (turbidite) formation | 3.0 | 0.3 | 0.01 | 0.047 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-30-6,59-61 | carbonate-siliceous-clayey (turbidite) formation | 4.2 | 0.3 | 0.03 | 0.031 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-31-1,6-9 | carbonate-siliceous-clayey (turbidite) formation | 5.8 | 0.5 | 0.01 | 0.038 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-34-2,25-27 | carbonate-siliceous-clayey (turbidite) formation | 7.5 | 0.5 | 0.01 | 0.047 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-34-6,2 9-3 1 | carbonate-siliceous-clayey (turbidite) formation | 7.6 | 0.6 | 0.03 | 0.047 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-36-5,74-76 | formation of speckled clays | 10.7 | 0.5 | 0.05 | 0.042 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-36-5,94-98 | formation of speckled clays | 10.4 | 0.6 | 0.04 | 0.042 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-37-3,8-9 | formation of speckled clays | 5.5 | 0.7 | 0.01 | 0.049 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-37-3,15-17 | formation of speckled clays | 5.1 | 0.7 | 0.01 | 0.059 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-38-1,31-32 | formation of speckled clays | 4.8 | 0.6 | 0.10 | 0.046 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-38-2,145-146 | formation of speckled clays | 6.3 | 0.7 | 0.09 | 0.040 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-38-2,145-150 | formation of speckled clays | 6.0 | 0.5 | 0.02 | 0.042 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-38-3,90-91 | formation of speckled clays | 5.6 | 0.7 | 0.04 | 0.053 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-39-1,129-131 | formation of speckled clays | 7.1 | 0.7 | 0.01 | 0.048 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-39-1,144-145 | formation of speckled clays | 7.2 | 0.8 | 0.10 | 0.040 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-40-2,0-1 | formation of speckled clays | 5.2 | 0.5 | 0.03 | 0.040 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-40-2,3-4 | formation of speckled clays | 6.8 | 1.0 | 0.05 | 0.035 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-41-4,68-70 | formation of speckled clays | 6.0 | 1.0 | 0.01 | 0.045 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-42-2,105-107 | formation of black clays | 1.7 | 0.5 | 0.25 | 0.029 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-44-3,23.5-24.5 | formation of black clays | 4.1 | 0.6 | 0.04 | 0.039 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-47-4,47-50 | formation of black clays | 6.4 | 0.5 | 0.03 | 0.050 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-48-3,123-124 | formation of black clays | 2.8 | 0.3 | 0.27 | 0.018 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-49-3,56-62 | formation of black clays | 5.3 | 0.5 | 0.01 | 0.038 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-49-3,90-93 | formation of black clays | 4.7 | 0.8 | 0.23 | 0.040 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-60-5,140-141 | formation of black clays | 5.0 | 0.8 | 0.04 | 0.044 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-63-4,19-23 | formation of black clays | 1.3 | 12.7 | 3.32 | 0.072 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-64-2,47-48 | formation of black clays | 4.6 | 2.0 | 0.01 | 0.037 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-64-2,79-80 | formation of black clays | 1.6 | 12.8 | 7.10 | 0.050 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-64-3,22-23 | formation of black clays | 3.7 | 1.3 | 0.01 | 0.060 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-64-3,24-25 | formation of black clays | 3.9 | 2.1 | 0.01 | 0.051 |
43-386 | 31.1868 | -64.2490 | -4782 | 43-386-65-3,104-105 | formation of black clays | 4.6 | 2.1 | 0.01 | 0.054 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-7-3,80-83 | carbonate-siliceous-clayey (turbidite) formation | 5.4 | 0.4 | 0.05 | 0.035 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-10-5,89-91 | carbonate-siliceous-clayey (turbidite) formation | 2.7 | 0.4 | 0.10 | 0.044 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-18-1,81-83 | carbonate-siliceous-clayey (turbidite) formation | 3.0 | 0.4 | 0.05 | 0.033 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-18-1,81-83 | carbonate-siliceous-clayey (turbidite) formation | 3.5 | 0.4 | 0.01 | 0.040 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-18-1,84-86 | carbonate-siliceous-clayey (turbidite) formation | 3.1 | 0.4 | 0.01 | 0.035 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-19-1,103-108 | carbonate-siliceous-clayey (turbidite) formation | 4.0 | 0.4 | 0.02 | 0.035 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-19-2,61-63 | carbonate-siliceous-clayey (turbidite) formation | 1.6 | 0.5 | 0.02 | 0.056 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-19-3,20-22 | carbonate-siliceous-clayey (turbidite) formation | 4.4 | 0.6 | 0.05 | 0.045 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-23-4,120-122 | carbonate-siliceous-clayey (turbidite) formation | 8.2 | 0.5 | 0.03 | 0.039 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-25-3,141-146 | carbonate-siliceous-clayey (turbidite) formation | 3.2 | 0.5 | 0.01 | 0.047 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-26-2,0-2 | carbonate-siliceous-clayey (turbidite) formation | 6.1 | 0.7 | 0.01 | 0.051 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-27-1,39-41 | carbonate-siliceous-clayey (turbidite) formation | 7.8 | 0.4 | 0.01 | 0.038 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-27-6,40-42 | pelagic carbonate formations | 4.8 | 0.3 | 0.02 | 0.050 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-28-1,131-133 | pelagic carbonate formations | 6.8 | 0.4 | 0.03 | 0.031 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-29-2,12-15 | formation of speckled clays | 11.5 | 0.5 | 0.01 | 0.042 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-29-4,101-106 | formation of speckled clays | 12.2 | 0.4 | 0.04 | 0.033 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-30-1,134-140 | formation of black clays | 2.5 | 1.2 | 0.01 | 0.048 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-34-4,117-119 | formation of black clays | 4.6 | 0.6 | 0.01 | 0.046 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-34-4,96-98 | formation of black clays | 4.8 | 0.5 | 0.01 | 0.046 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-35-5,0-2 | formation of black clays | 6.8 | 0.4 | 0.01 | 0.047 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-37-2,101-103 | formation of black clays | 5.1 | 0.6 | 0.01 | 0.043 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-42-1,72-75 | ancient carbonate formation (gray-colored sub-formation) | 2.4 | 1.0 | 0.01 | 0.054 |
43-387 | 32.3200 | -67.6667 | -5117 | 43-387-50-1,35-38 | ancient carbonate formation (gray-colored sub-formation) | 8.3 | 0.6 | 0.01 | 0.074 |
44-388A | 35.5222 | -69.3960 | -4919 | 44-388A-2-3,0-3 | terrigenous turbidite formation | 6.5 | 0.6 | 0.01 | 0.093 |
44-390 | 30.1423 | -76.1123 | -2665 | 44-390-3-1,146-148 | pelagic carbonate formations | 8.4 | 0.6 | 0.01 | 0.071 |
44-390A | 30.1423 | -76.1123 | -2665 | 44-390A-14-5,144-147 | pelagic carbonate formations | 4.0 | 0.7 | 0.01 | 0.120 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-17-4,139-142 | siliceous-carbonate avalanche formation of the Blake-Bahama Basin | 4.9 | 0.6 | 0.01 | 0.051 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-20-2,54-57 | siliceous-carbonate avalanche formation of the Blake-Bahama Basin | 6.7 | 0.6 | 0.01 | 0.045 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-1,47-50 | formation of speckled clays | 9.3 | 0.4 | 0.46 | 0.116 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-1,63-67 | formation of speckled clays | 10.3 | 0.4 | 0.01 | 0.116 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-1,75-79 | formation of speckled clays | 11.5 | 0.4 | 0.07 | 0.099 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-1,88-89 | formation of speckled clays | 10.2 | 0.9 | 0.01 | 0.106 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-2,90-91 | formation of speckled clays | 11.0 | 0.6 | 0.01 | 0.098 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-3,93-96 | formation of speckled clays | 8.7 | 0.7 | 0.01 | 0.048 |
44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-21-5,8-10 | formation of speckled clays | 10.2 | 0.4 | 0.01 | 0.128 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-2-1,6-10 | siliceous-carbonate avalanche formation of the Blake-Bahama Basin | 2.1 | 0.5 | 0.01 | 0.052 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-4-1,107-110 | formation of speckled clays | 9.5 | 0.5 | 0.01 | 0.047 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-5-1,72-75 | formation of speckled clays | 9.1 | 0.7 | 0.01 | 0.050 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-6-1,56-61 | formation of speckled clays | 9.1 | 0.6 | 0.01 | 0.044 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-6-5,104-109 | formation of black clays | 10.5 | 0.5 | 0.01 | 0.044 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-7-1,16-18 | formation of black clays | 10.3 | 0.5 | 0.01 | 0.048 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-8-1,102-105 | formation of black clays | 10.1 | 0.5 | 0.01 | 0.038 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-9-2,5-8 | formation of black clays | 3.8 | 4.4 | 0.07 | 0.127 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-10-1,72-74 | formation of black clays | 10.0 | 0.4 | 0.01 | 0.106 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-10-2,108-111 | formation of black clays | 10.0 | 0.6 | 0.01 | 0.120 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-10-2,108-111 | formation of black clays | 9.4 | 0.4 | 0.01 | 0.141 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-28-2,106-110 | ancient carbonate formation (gray-colored sub-formation) | 6.1 | 0.7 | 0.01 | 0.051 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-15-3,83-86 | ancient carbonate formation (gray-colored sub-formation) | 6.2 | 0.6 | 0.01 | 0.055 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-24-1,115-117 | ancient carbonate formation (gray-colored sub-formation) | 7.6 | 0.4 | 0.01 | 0.061 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-24-6,35-68 | ancient carbonate formation (gray-colored sub-formation) | 5.1 | 0.6 | 0.01 | 0.063 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-26-2,63-65 | ancient carbonate formation (gray-colored sub-formation) | 2.6 | 0.7 | 0.02 | 0.050 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-45-3,71-77 | ancient carbonate formation (red-colored sub-formation) | 0.9 | 0.6 | 0.06 | |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-46-1,139-142 | ancient carbonate formation (red-colored sub-formation) | 6.6 | 0.7 | 0.01 | 0.045 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-47-1,41-43 | ancient carbonate formation (red-colored sub-formation) | 3.7 | 0.5 | 0.13 | 0.043 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-49-2,137-139 | ancient carbonate formation (red-colored sub-formation) | 8.0 | 0.7 | 0.01 | 0.045 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-49-2,137-139 | ancient carbonate formation (red-colored sub-formation) | 7.6 | 0.7 | 0.01 | 0.055 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-49-2,81-83 | ancient carbonate formation (red-colored sub-formation) | 4.7 | 0.9 | 0.01 | 0.055 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-50-1,118-120 | ancient carbonate formation (red-colored sub-formation) | 5.0 | 0.6 | 0.03 | 0.084 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-52-2,103-106 | ancient carbonate formation (red-colored sub-formation) | 6.8 | 0.6 | 0.01 | 0.034 |
44-391C | 28.2268 | -75.6167 | -4974 | 44-391C-52-4,13-15 | ancient carbonate formation (red-colored sub-formation) | 5.5 | 1.1 | 0.01 | 0.055 |