Murdmaa, Ivar O; Kazakova, Vera P; Rudakova, Alevtina N (1979): (Table 6) Light mineral composition of 0.05-0.01 mm grain size fraction from sedimentary and volcano-sedimentary rocks drilled in DSDP Legs 43 and 44 [dataset]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.733289, 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.
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Murdmaa, Ivar O; Kazakova, Vera P; Rudakova, Alevtina N (1979): Mineral composition of sedimentary and volcano-sedimentary rocks. In: Bezrukov, P.L. (Ed.), Geological Formations of the Southwest Atlantic Ocean; Nauka Publ. (Moscow): in Russian, 67-95
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 33.557250 * Median Longitude: -66.322750 * South-bound Latitude: 28.226800 * West-bound Longitude: -76.112300 * North-bound Latitude: 40.360800 * East-bound Longitude: -51.663300
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
43-383 * Latitude: 39.248000 * Longitude: -53.353000 * Date/Time: 1975-07-10T00:00:00 * Elevation: -5283.0 m * Penetration: 120.3 m * Recovery: 4.9 m * Location: North Atlantic/RIDGE * Campaign: Leg43 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 1 cores; 9.6 m cored; 9.5 m drilled; 51 % recovery
43-384 * Latitude: 40.360800 * Longitude: -51.663300 * Date/Time: 1975-07-12T00:00:00 * Elevation: -3909.0 m * Penetration: 330.3 m * Recovery: 110.7 m * Location: North Atlantic/RIDGE * Campaign: Leg43 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 21 cores; 185 m cored; 9.3 m drilled; 59.8 % recovery
Comment:
Data calculated from numbers of mineral grains. <1% = single grains.
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 | Sample comment | Sample comment | Murdmaa, Ivar O | |||
| 8 | Quartz | Qz | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 9 | Kalifeldspar | Kfs | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 10 | Feldspar | Fsp | % | Murdmaa, Ivar O | Counting, Stereo Microscope | basic |
| 11 | Mica | Mica | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 12 | Volcanic glass, acidic | Volc glass acidic | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 13 | Volcanic components | Volcanic | % | Murdmaa, Ivar O | Counting, Stereo Microscope | basic |
| 14 | Palagonite | Palagonite | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 15 | Chlorite | Chl | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 16 | Zeolite | Zeo | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 17 | Glauconite | Glt | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 18 | Chalcedony | Chalcedony | % | Murdmaa, Ivar O | Counting, Stereo Microscope | + cristobalite |
| 19 | Gypsum | Gp | % | Murdmaa, Ivar O | Counting, Stereo Microscope | |
| 20 | Carbonates | Carb | % | Murdmaa, Ivar O | Counting, Stereo Microscope | unidentified |
| 21 | Calcite | Cal | % | Murdmaa, Ivar O | Counting, Stereo Microscope | biogenic |
| 22 | Opal particles | Opal | % | Murdmaa, Ivar O | Counting, Stereo Microscope | biogenic |
| 23 | Phosphate | PO4 | % | Murdmaa, Ivar O | Counting, Stereo Microscope | biogenic |
| 24 | Minerals | Minerals | % | Murdmaa, Ivar O | Counting, Stereo Microscope | difficult identified grains |
| 25 | Comment | Comment | Murdmaa, Ivar O | |||
| 26 | Quartz/Feldspar ratio | Qz/Fsp | Murdmaa, Ivar O | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2786 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Formation | 7 Sample comment | 8 Qz [%] | 9 Kfs [%] | 10 Fsp [%] | 11 Mica [%] | 12 Volc glass acidic [%] | 13 Volcanic [%] | 14 Palagonite [%] | 15 Chl [%] | 16 Zeo [%] | 17 Glt [%] | 18 Chalcedony [%] | 19 Gp [%] | 20 Carb [%] | 21 Cal [%] | 22 Opal [%] | 23 PO4 [%] | 24 Minerals [%] | 25 Comment | 26 Qz/Fsp |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-1-2,60-62 | terrigenous turbidite formation | 42 | 16 | <1 | 1 | 0 | 0 | 0 | 1 | 0 | 11 | 1 | 0 | 0 | 12 | 0 | 0 | 16 | 2.6 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-1-3,126-128 | terrigenous turbidite formation | 51 | 18 | 1 | <1 | 0 | 0 | 0 | <1 | 0 | 12 | 0 | 0 | 0 | 7 | 0 | 0 | 10 | 2.7 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-1-4,90-92 | terrigenous turbidite formation | 40 | 20 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 17 | 0 | 0 | 18 | 2.0 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-1-6,40-42 | terrigenous turbidite formation | 46 | 23 | <1 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 17 | 0 | 0 | 12 | 2.0 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-2-1,60-70 | terrigenous turbidite formation | 48 | 18 | <1 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 0 | 0 | 7 | <1 | 0 | 20 | 2.7 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-2-3,48-50 | terrigenous turbidite formation | 48 | 23 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 0 | 0 | 6 | 0 | 0 | 17 | 2.0 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-2-3,64-66 | terrigenous turbidite formation | 52 | 18 | 1 | <1 | 0 | 0 | 0 | 0 | <1 | 5 | 0 | 0 | 0 | 6 | 0 | 0 | 18 | 2.7 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-2-3,92-94 | terrigenous turbidite formation | 49 | 23 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 4 | 1 | 0 | 0 | 4 | 0 | 0 | 17 | 2.1 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-3-2,100-102 | terrigenous turbidite formation | 54 | 20 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 7 | 0 | 0 | 18 | 2.6 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-3-2,147-149 | terrigenous turbidite formation | 46 | 20 | 0 | 0 | 0 | 0 | 0 | 1 | <1 | 8 | 3 | 0 | 0 | 6 | 0 | 0 | 16 | 2.3 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-5-3,100-102 | hemipelagic clayey formation | 50 | 22 | 0 | 2 | <1 | 0 | 0 | 1 | 1 | 2 | 0 | 0 | 0 | 4 | <1 | 3 | 14 | 2.3 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-6-2,148-150 | hemipelagic clayey formation | 55 | 20 | <1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 3 | 13 | 2.8 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-7-1,43-45 | hemipelagic clayey formation | 45 | 25 | 1 | 0 | 1 | <1 | 0 | <1 | <1 | 1 | 0 | 0 | 0 | 2 | <1 | 4 | 17 | 1.8 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-7-6,67-69 | hemipelagic clayey formation | 17 | 7 | 0 | 0 | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 13 | 1 | 2.4 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-8-5,97-99 | hemipelagic clayey formation | 34 | 9 | 0 | 0 | 0 | 0 | 0 | 2 | <1 | 2 | <1 | 0 | 30 | 0 | 0 | 15 | 8 | 3.8 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-9-1,100-102 | hemipelagic clayey formation | 50 | 20 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 4 | 2 | 0 | 8 | 15 | 2.5 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-11-4,76-78 | hemipelagic clayey formation | 44 | 15 | 0 | 0 | <1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 24 | 16 | 2.3 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-12-4,103-105 | hemipelagic clayey formation | 34 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | 1 | 1 | 33 | 25 | 5 | 17.0 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-13-1,34-36 | hemipelagic clayey formation | 13 | 5 | <1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 15 | 47 | 12 | 2.6 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-14-5,123-125 | hemipelagic clayey formation | 14 | 4 | <1 | <1 | 1 | 0 | 0 | 3 | 1 | 1 | 0 | 0 | 2 | 0 | 7 | 33 | 33 | 3.4 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-15-4,10-12 | formation of speckled clays | 12 | 3 | <1 | 0 | <1 | 0 | 1 | 11 | 5 | <1 | 0 | 0 | 0 | 20 | 0 | 14 | 33 | 3.1 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-15-6,8-10 | formation of speckled clays | 4 | 1 | <1 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 54 | 31 | 3.2 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-1,130-134 | volcanoclastic formation of the New England Seamount Chain | 0 | 1 | 0 | 0 | 0 | 0 | <1 | 2 | 62 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 30 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-2,46-49 | volcanoclastic formation of the New England Seamount Chain | <1 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 85 | 0.1 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-3,63-65 | volcanoclastic formation of the New England Seamount Chain | <1 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 23 | 0 | 0 | 26 | 0 | 16 | 0 | 0 | 31 | 0.2 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-5,94 | volcanoclastic formation of the New England Seamount Chain | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 90 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-6,38-41 | volcanoclastic formation of the New England Seamount Chain | 1 | <1 | 0 | 0 | 0 | 0 | 1 | <1 | 14 | 0 | 0 | 0 | 0 | 70 | 0 | 3 | 10 | 4.0 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-6,47-60 | volcanoclastic formation of the New England Seamount Chain | <1 | 0 | 0 | 0 | <1 | 0 | 44 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-16-6,124-126 | volcanoclastic formation of the New England Seamount Chain | 0 | <1 | 0 | 0 | 0 | 0 | 1 | <1 | 26 | 0 | 0 | 0 | 0 | 28 | 1 | 0 | 47 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-2,35-39 | volcanoclastic formation of the New England Seamount Chain | 0 | <1 | 0 | 0 | 0 | 0 | 4 | 2 | 28 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 64 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-2,119-121 | volcanoclastic formation of the New England Seamount Chain | <1 | 0 | 0 | 0 | 0 | 0 | 19 | 0 | 48 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 30 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-3,30-35 | volcanoclastic formation of the New England Seamount Chain | 0 | 1 | 0 | 0 | 0 | 0 | 4 | 6 | 21 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 59 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-3,34 | volcanoclastic formation of the New England Seamount Chain | 0 | 2 | 0 | 0 | 0 | 0 | 4 | 6 | 1 | 0 | 0 | 0 | 0 | 21 | 0 | 0 | 66 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-3,61-63 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 33 | 0 | 24 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 36 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-5,63-66 | volcanoclastic formation of the New England Seamount Chain | 1 | 1 | 0 | 0 | 0 | 0 | 0 | <1 | 38 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 59 | 1.5 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-6,50 | volcanoclastic formation of the New England Seamount Chain | <1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 30 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 43 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-17-6,100-102 | volcanoclastic formation of the New England Seamount Chain | 2 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 83 | 0.3 | ||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-1,108 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 4 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 83 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-2,36 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 38 | 0 | 0 | 60 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-4,30-40 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 88 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-4,129-133 | volcanoclastic formation of the New England Seamount Chain | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 0 | 19 | 0 | 0 | 0 | 75 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-18-4,137 | volcanoclastic formation of the New England Seamount Chain | 0 | <1 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 9 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-19-2,9-11 | volcanoclastic formation of the New England Seamount Chain | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 16 | 0 | 0 | 0 | 0 | 56 | 0 | 0 | 28 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-19-2,21-23 | volcanoclastic formation of the New England Seamount Chain | 0 | 1 | 0 | 0 | 0 | 0 | 5 | <1 | 11 | 0 | 0 | 0 | 9 | 0 | 0 | 0 | 73 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-20-2,114 | volcanoclastic formation of the New England Seamount Chain | 0 | <1 | 0 | 0 | 0 | 0 | 1 | 4 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 83 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-20-4,36-41 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 7 | 0 | 0 | 0 | 0 | 9 | 0 | 0 | 84 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-20-5,78-80 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 48 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 48 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-21-1,122 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 61 | 26 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-21-2,80 | volcanoclastic formation of the New England Seamount Chain | <1 | 1 | 0 | 0 | 0 | 0 | 2 | 5 | 2 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 85 | |||
| 43-382 | 34.4173 | -56.5375 | -5526 | 43-382-21-3,123 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 7 | 4 | 0 | 0 | 0 | 0 | 2 | <1 | 0 | 86 | |||
| 43-383 | 39.2480 | -53.3530 | -5283 | 43-383-1-2,30-33 | terrigenous turbidite formation | 43 | 22 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | <1 | 0 | 0 | 0 | 12 | 0 | 0 | 23 | 1.9 | ||
| 43-383 | 39.2480 | -53.3530 | -5283 | 43-383-1-2,140-144 | terrigenous turbidite formation | 48 | 19 | <1 | 1 | 0 | 0 | 0 | 1 | 0 | <1 | 0 | 0 | 0 | 14 | 0 | 0 | 18 | 2.5 | ||
| 43-383 | 39.2480 | -53.3530 | -5283 | 43-383-1-4,15-19 | terrigenous turbidite formation | 42 | 20 | 0 | <1 | 0 | 0 | 0 | <1 | 0 | <1 | 0 | 0 | 0 | 10 | 0 | 0 | 25 | 2.1 | ||
| 43-384 | 40.3608 | -51.6633 | -3909 | 43-384-1-3,130-133 | pelagic carbonate formations | <1 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | 2 | <1 | 0 | 0 | 0 | 77 | 18 | 1 | 0 | |||
| 43-384 | 40.3608 | -51.6633 | -3909 | 43-384-2-4,38-40 | pelagic carbonate formations | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | <1 | 0 | 0 | 0 | 86 | 6 | 6 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-1-1,102-104 | hemipelagic clayey formation | 33 | 6 | <1 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 0 | 0 | 49 | 0 | 0 | 6 | 5.5 | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-1-4,100 | hemipelagic clayey formation | 50 | 14 | <1 | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 0 | 0 | 0 | 1 | 2 | 6 | 19 | 3.6 | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-2-2,31-33 | hemipelagic clayey formation | 6 | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | <1 | 0 | 0 | 0 | 48 | 4 | 6 | 4 | 5.2 | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-4-2,100 | carbonaceous-siliceous-clayey (turbidite) formation | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 94 | 2 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-5-2,110-112 | carbonaceous-siliceous-clayey (turbidite) formation | 5 | <1 | <1 | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | 4 | 46 | 44 | 0 | 6.0 | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-8-5,88 | formation of speckled clays | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-9-1,94 | formation of speckled clays | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 96 | 0 | 0 | 0 | 0 | <1 | 1 | 2 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-10-1,109-111 | formation of speckled clays | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-11-1,120-123 | formation of speckled clays | <1 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-12-2,31-33 | formation of speckled clays | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 6 | 0 | 7 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-13-3,84-87 | formation of speckled clays | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 4 | 37 | 0 | 0 | 14 | 0 | 33 | 6 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-13-4,54-56 | formation of speckled clays | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 7 | 0 | 26 | 0 | 0 | 31 | 0 | 32 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-14-1,68-72 | formation of speckled clays | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 12 | 32 | <1 | 45 | 7 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-15-1,94-97 | formation of speckled clays | 2 | 1 | 0 | 0 | 0 | 0 | <1 | <1 | 4 | <1 | 12 | 0 | 0 | 10 | 0 | 13 | 57 | 1.7 | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-15-3,77-80 | formation of speckled clays | 0 | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 26 | <1 | 28 | 0 | 0 | 20 | 0 | 18 | 3 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,75 | volcanoclastic formation of the New England Seamount Chain | <1 | 0 | 0 | 0 | 0 | 0 | 18 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 69 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,94-96 | volcanoclastic formation of the New England Seamount Chain | 13 | 4 | 1 | 0 | 0 | 0 | 9 | 0 | <1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 70 | 2.8 | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,121-124 | volcanoclastic formation of the New England Seamount Chain | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | 0 | 80 | phosphate grains occur | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,132-134 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | <1 | 0 | 0 | 12 | 0 | 6 | 1 | 2 | 66 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-16-2,137-140 | volcanoclastic formation of the New England Seamount Chain | 8 | 3 | 0 | 0 | 0 | 14 | 17 | 0 | 1 | 0 | 0 | 0 | 0 | <1 | 0 | 0 | 58 | 2.6 | ||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-19-1,121-123 | volcanoclastic formation of the New England Seamount Chain | 0 | 0 | 0 | 0 | 0 | 21 | 78 | 0 | 1 | 0 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | |||
| 43-385 | 37.3695 | -60.1575 | -4936 | 43-385-19-CC | volcanoclastic formation of the New England Seamount Chain | <1 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 78 | phosphate grains occur | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-1-3,74-76 | pelagic carbonate formations | 6 | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | 0 | 0 | 93 | 0 | 0 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-2-1,140-142 | hemipelagic clayey formation | 43 | 9 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 19 | 0 | 0 | 28 | 4.8 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-3-1,147-150 | hemipelagic clayey formation | 31 | 10 | 1 | 0 | 0 | 0 | 0 | 6 | <1 | 1 | 0 | 0 | 0 | 15 | 0 | 10 | 25 | 2.7 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-1,106 | basalt-greywacke formation of the Bermuda massife | <1 | <1 | 0 | 1 | 0 | 0 | 0 | 18 | 1 | 0 | 0 | 0 | 0 | 57 | 1 | 5 | 16 | 0.2 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-1,134-136 | basalt-greywacke formation of the Bermuda massife | 2 | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6.0 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-2,0-3 | basalt-greywacke formation of the Bermuda massife | 11 | 3 | 0 | <1 | 0 | 0 | <1 | 0 | 2 | 1 | 0 | 0 | 0 | 2 | 0 | 6 | 74 | 4.0 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-4,50 | basalt-greywacke formation of the Bermuda massife | <1 | 4 | 0 | 0 | 0 | 0 | 0 | 8 | 11 | 0 | 0 | 0 | 0 | 0 | 0 | 17 | 59 | 0.1 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-6,82 | basalt-greywacke formation of the Bermuda massife | 2 | 8 | 0 | 2 | 0 | 0 | 0 | 22 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 61 | 0.3 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-4-6,82-89 | basalt-greywacke formation of the Bermuda massife | 0 | 3 | 0 | 3 | 0 | 0 | 1 | 28 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 58 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-5-1,60-62 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 14 | 4 | 0 | 0 | 0 | 0 | 13 | 0 | 0 | 64 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-5-2,6 | basalt-greywacke formation of the Bermuda massife | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 9 | 3 | 0 | 0 | 0 | 0 | 48 | 2 | 5 | 26 | 0.2 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-5-2,33-35 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 17 | 11 | 0 | 0 | 0 | 0 | 22 | 0 | 0 | 48 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-5-2,90-92 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 21 | 3 | <1 | 0 | 0 | 0 | 30 | 0 | 0 | 46 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-5-2,102 | basalt-greywacke formation of the Bermuda massife | <1 | 1 | 0 | 0 | 0 | 0 | 0 | 18 | 12 | 0 | 0 | 0 | 0 | 23 | 2 | 0 | 44 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-5-2,105-107 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 14 | 0 | 1 | 0 | 0 | 19 | 1 | 0 | 50 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-5-4,120-122 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 20 | 3 | 0 | 0 | 0 | 0 | 21 | 0 | 0 | 55 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-6-1,99 | basalt-greywacke formation of the Bermuda massife | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 18 | 3 | 0 | 0 | 0 | 0 | 17 | <1 | 0 | 59 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-6-1,104-106 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 12 | 8 | 0 | 0 | 0 | 0 | 15 | <1 | 0 | 56 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-7-2,54-58 | basalt-greywacke formation of the Bermuda massife | <1 | <1 | 0 | 0 | 0 | 0 | 0 | 11 | 8 | 0 | 0 | 0 | 0 | 8 | <1 | 0 | 72 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-7-4,139 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 9 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 54 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-8-5,101 | basalt-greywacke formation of the Bermuda massife | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 10 | 4 | 0 | 0 | 0 | 0 | 18 | <1 | 0 | 67 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-9-2,7 | basalt-greywacke formation of the Bermuda massife | 0 | 1 | 0 | 1 | 0 | 0 | 8 | 0 | 5 | 0 | 0 | 0 | 0 | 22 | 1 | 0 | 62 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-12-1,57-59 | basalt-greywacke formation of the Bermuda massife | 2 | <1 | <1 | 0 | 0 | 0 | 0 | 16 | 4 | 0 | 0 | 0 | 0 | 42 | 0 | 1 | 34 | 2.0 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-12-2,69 | basalt-greywacke formation of the Bermuda massife | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 31 | 6 | 0 | 0 | 0 | 0 | 13 | 1 | 0 | 48 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-15-1,0-2 | carbonaceous-siliceous-clayey (turbidite) formation | 7 | 1 | 0 | 0 | 1 | 0 | 0 | 11 | 13 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 63 | 5.7 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-15-1,93-97 | carbonaceous-siliceous-clayey (turbidite) formation | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 4 | 0 | 0 | 88 | 0 | 0 | 4 | 0 | 0 | 0 | 2.3 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-15-2,5 | carbonaceous-siliceous-clayey (turbidite) formation | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 88 | 0 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-15-2,12-13 | carbonaceous-siliceous-clayey (turbidite) formation | 9 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 32 | 55 | 0 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-15-2,14-17 | carbonaceous-siliceous-clayey (turbidite) formation | 13 | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 40 | 38 | 4 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-16-5,107 | carbonaceous-siliceous-clayey (turbidite) formation | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 92 | 1 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-17-1,74 | carbonaceous-siliceous-clayey (turbidite) formation | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 13 | 82 | 0 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-17-1,129 | carbonaceous-siliceous-clayey (turbidite) formation | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 36 | 56 | 0 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-17-1,130-135 | carbonaceous-siliceous-clayey (turbidite) formation | 16 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 51 | 30 | 0 | 0 | 16.0 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-17-2,82 | carbonaceous-siliceous-clayey (turbidite) formation | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 70 | 0 | 0 | |||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-17-4,63-66 | carbonaceous-siliceous-clayey (turbidite) formation | 6 | 1 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 1 | 0 | 0 | 0 | 48 | 44 | 0 | 0 | 6.0 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-41-4,71-73 | formation of speckled clays | 8 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 4 | 0 | 0 | 50 | 19 | 15 | 0 | 2.7 | ||
| 43-386 | 31.1868 | -64.2490 | -4782 | 43-386-38-5,81-83 | formation of speckled clays | 2 | 0 | 0 | 0 | 0 | 0 | 0 | <1 | 90 | 1 | 0 | 0 | 0 | 0 | 6 | 1 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-2-5,10-12 | carbonaceous-siliceous-clayey (turbidite) formation | 4 | 1 | 0 | <1 | 0 | 0 | <1 | 13 | 0 | 0 | 0 | 0 | 0 | 18 | 21 | 6 | 37 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-4-1,80-82 | carbonaceous-siliceous-clayey (turbidite) formation | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 94 | 6 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-6-3,49 | carbonaceous-siliceous-clayey (turbidite) formation | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-6-CC | carbonaceous-siliceous-clayey (turbidite) formation | 1 | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 98 | 1 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-7-1,35-38 | carbonaceous-siliceous-clayey (turbidite) formation | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 11 | 4 | 0 | 0 | 0 | 0 | 18 | 26 | 0 | 10 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-7-1,70-74 | carbonaceous-siliceous-clayey (turbidite) formation | 1 | 0 | 0 | 0 | <1 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 94 | 2 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-7-1,100 | carbonaceous-siliceous-clayey (turbidite) formation | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 96 | 1 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-7-5,70 | carbonaceous-siliceous-clayey (turbidite) formation | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 99 | 1 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-9-2,80 | carbonaceous-siliceous-clayey (turbidite) formation | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 98 | 1 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-9-3,117-120 | carbonaceous-siliceous-clayey (turbidite) formation | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 77 | 10 | 10 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-9-6,30 | carbonaceous-siliceous-clayey (turbidite) formation | 12 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 74 | 3 | 0 | 4.0 | ||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-10-5,70 | carbonaceous-siliceous-clayey (turbidite) formation | <1 | <1 | 2 | <1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 6 | 88 | 2 | 0 | |||
| 43-387 | 32.3200 | -67.6667 | -5117 | 43-387-26-1,48-50 | carbonaceous-siliceous-clayey (turbidite) formation | 6 | 2 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | 0 | 0 | 0 | 91 | 0 | 0 | |||
| 44-388 | 35.5222 | -69.3960 | -4919 | 44-388-1-2,aver. | terrigenous turbidite formation | 37 | 10 | 0 | <1 | 0 | 0 | 0 | <1 | 0 | 2 | 0 | 0 | 0 | 42 | 0 | 0 | 9 | 3.7 | ||
| 44-388A | 35.5222 | -69.3960 | -4919 | 44-388A-9-3,38-41 | hemipelagic clayey formation | 24 | 8 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 0 | 0 | 0 | 45 | 2 | 1 | 8 | 12 | 2.9 | ||
| 44-388A | 35.5222 | -69.3960 | -4919 | 44-388A-9-5,110-113 | hemipelagic clayey formation | 14 | 4 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 1 | 0 | 0 | 58 | 1 | 1 | 6 | 8 | 3.4 | ||
| 44-390 | 30.1423 | -76.1123 | -2665 | 44-390-1-2,147 | pelagic carbonate formations | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 93 | 0 | 0 | 5 | 0 | 0 | 0 | |||
| 44-390 | 30.1423 | -76.1123 | -2665 | 44-390-1-6,115-117 | pelagic carbonate formations | residue insoluble in 10% HCl | 10 | 6 | 0 | 0 | 0 | 0 | 0 | 16 | 18 | <1 | 0 | 0 | 0 | 0 | 1 | 0 | 48 | ||
| 44-390 | 30.1423 | -76.1123 | -2665 | 44-390-3-2,94-96 | pelagic carbonate formations | residue insoluble in 10% HCl | 10 | 14 | 0 | 0 | 1 | 0 | 0 | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 5 | 0 | 62 | 0.8 | |
| 44-390 | 30.1423 | -76.1123 | -2665 | 44-390-4-1,135-139 | pelagic carbonate formations | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 3 | 0 | |||
| 44-390 | 30.1423 | -76.1123 | -2665 | 44-390-8-3,68-74 | pelagic carbonate formations | 2 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 19 | 0 | 0 | 76 | 1.6 | ||
| 44-390A | 30.1423 | -76.1123 | -2665 | 44-390A-1-2,137-141 | pelagic carbonate formations | <1 | <1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 96 | 0 | 2 | 0 | |||
| 44-391 | 28.2288 | -75.6127 | -4974 | 44-391-1-1,67-70 | hemipelagic clayey formation | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 91 | 0 | 0 | 0 | 4.1 | ||
| 44-391 | 28.2288 | -75.6127 | -4974 | 44-391-1-1,67-70 | hemipelagic clayey formation | insoluble in 10% HCl residue analyzed | 35 | 9 | 0 | 0 | 0 | <1 | 0 | 9 | 1 | 0 | 0 | 0 | 0 | 0 | 9 | 0 | 36 | 3.8 | |
| 44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-1-1,74-77 | hemipelagic clayey formation | 12 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 76 | 2 | 2 | 0 | 2.0 | ||
| 44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-1-6,96-99 | hemipelagic clayey formation | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 20 | 72 | 0 | 0 | 2 | 1.3 | ||
| 44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-4-1,12-15 | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | 3 | 4 | 0 | 0 | 0 | 0 | 0 | <1 | 0 | 2 | 0 | 0 | 0 | 89 | 0 | 0 | 2 | 0.9 | ||
| 44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-4-CC | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | 45 | 14 | 0 | 0 | <1 | 0 | 0 | 0 | 0 | 16 | 0 | 0 | 0 | 4 | 14 | 1 | 4 | 3.2 | ||
| 44-391A | 28.2268 | -75.6167 | -4974 | 44-391A-5-1,70-73 | siliceous-caerbonaceous (avalanche) formation of the Blake-Bahama Basin | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 94 | 0 | 0 | 1 | 3.0 |