Karpoff, Anne Marie; Destrigneville, Christine; Bartier, Danièle; Déjardin, Pascale (2002): (Table 2) Mineralogical composition of the clay-rich intervals from ODP Sites 166-1006 and 166-1007 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.744031, In supplement to: Karpoff, AM et al. (2002): Phyllosilicates and zeolite assemblages in the carbonate periplatform of the Great Bahama Bank: origin and relation to diagenetic processes (ODP Leg 166, Sites 1006 and 1007). Marine Geology, 185(1-2), 55-74, https://doi.org/10.1016/S0025-3227(01)00290-0
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 24.469467 * Median Longitude: -79.367933 * South-bound Latitude: 24.399800 * West-bound Longitude: -79.459000 * North-bound Latitude: 24.504400 * East-bound Longitude: -79.322300
Date/Time Start: 1996-03-20T05:54:00 * Date/Time End: 1996-04-08T15:18:00
Minimum DEPTH, sediment/rock: 18.98 m * Maximum DEPTH, sediment/rock: 1208.70 m
Event(s):
166-1006A * Latitude: 24.399800 * Longitude: -79.459000 * Date/Time Start: 1996-03-20T05:54:00 * Date/Time End: 1996-03-24T04:40:00 * Elevation: -657.9 m * Penetration: 717.3 m * Recovery: 646.93 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 77 cores; 717.3 m cored; 0 m drilled; 90.2 % recovery
166-1007B * Latitude: 24.504400 * Longitude: -79.322300 * Date/Time Start: 1996-03-29T06:30:00 * Date/Time End: 1996-03-30T17:45:00 * Elevation: -647.4 m * Penetration: 377.7 m * Recovery: 198.42 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 41 core; 375.7 m cored; 0 m drilled; 52.8 % recovery
166-1007C * Latitude: 24.504200 * Longitude: -79.322500 * Date/Time Start: 1996-03-30T17:45:00 * Date/Time End: 1996-04-08T15:18:00 * Elevation: -647.3 m * Penetration: 1235.4 m * Recovery: 503.27 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 97 cores; 933.4 m cored; 0 m drilled; 53.9 % recovery
Comment:
Depth = mbsf
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Sample code/label | Sample label | Karpoff, Anne Marie | DSDP/ODP/IODP sample designation | ||
3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
4 | Lithologic unit/sequence | Unit | Karpoff, Anne Marie | unit | ||
5 | Lithologic unit/sequence | Unit | Karpoff, Anne Marie | sequence | ||
6 | Chlorite | Chl | % | Karpoff, Anne Marie | X-ray diffraction, clay fraction | |
7 | Kaolinite | Kln | % | Karpoff, Anne Marie | X-ray diffraction, clay fraction | |
8 | Illite | Ill | % | Karpoff, Anne Marie | X-ray diffraction, clay fraction | <1 = traces |
9 | Smectite | Sme | % | Karpoff, Anne Marie | X-ray diffraction, clay fraction | |
10 | Illite mixed layer (10-14Å) | Ill m l | % | Karpoff, Anne Marie | X-ray diffraction, clay fraction | IS = mixed layers illite-smectite, <1 = traces |
11 | Minerals | Minerals | Karpoff, Anne Marie | X-ray diffraction, clay fraction | others | |
12 | Clinoptilolite | Cpt | Karpoff, Anne Marie | X-ray diffraction, clay fraction | traced by a peak at 9Arelative abundance low (+) to high (+++++) | |
13 | Ratio | Ratio | Karpoff, Anne Marie | X-ray diffraction, clay fraction | (kaolinite + illite)/(IS + smectite) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
268 data points
Data
1 Event | 2 Sample label (DSDP/ODP/IODP sample designation) | 3 Depth sed [m] | 4 Unit (unit) | 5 Unit (sequence) | 6 Chl [%] (X-ray diffraction, clay fraction) | 7 Kln [%] (X-ray diffraction, clay fraction) | 8 Ill [%] (<1 = traces, X-ray diffractio...) | 9 Sme [%] (X-ray diffraction, clay fraction) | 10 Ill m l [%] (IS = mixed layers illite-smec...) | 11 Minerals (others, X-ray diffraction, cl...) | 12 Cpt (traced by a peak at 9Arelativ...) | 13 Ratio ((kaolinite + illite)/(IS + sm...) |
---|---|---|---|---|---|---|---|---|---|---|---|---|
166-1006A | 166-1006A-3H-2,88-91 | 18.98 | IB | c | 15 | 20 | 50 | 5 | 10 | quartz, feldspar, palygorskite | 4.67 | |
166-1006A | 166-1006A-3H-2,102-105 | 19.12 | IB | c | 20 | 15 | 45 | 15 | 5 | quartz, feldspar, palygorskite | 3.00 | |
166-1006A | 166-1006A-6H-2,55-57 | 47.15 | IB | c | 20 | 25 | 35 | 15 | 5 | quartz, feldspar, palygorskite | 3.00 | |
166-1006A | 166-1006A-6H-2,65-67 | 47.25 | IB | c | 20 | 30 | 30 | 10 | 10 | quartz, feldspar, palygorskite | 3.00 | |
166-1006A | 166-1006A-6H-5,132-134 | 52.42 | IB | c | 20 | 25 | 40 | 10 | 5 | quartz, feldspar, palygorskite | 4.33 | |
166-1006A | 166-1006A-14H-1,12-14 | 121.22 | IB | d | 10 | 20 | 20 | 50 | palygorskite | 0.80 | ||
166-1006A | 166-1006A-14H-1,23-25 | 121.33 | IB | d | 15 | 20 | 20 | 45 | palygorskite | 0.89 | ||
166-1006A | 166-1006A-14H-3,49-51 | 124.59 | IB | d | 15 | 20 | 10 | 55 | <1 | palygorskite | 0.55 | |
166-1006A | 166-1006A-14H-3,53-55 | 124.63 | IB | d | 15 | 15 | 15 | 55 | palygorskite | 0.55 | ||
166-1007B | 166-1007B-5H-4,57-59 | 45.07 | IC | d | 20 | 10 | 15 | 55 | <1 | palygorskite | 0.45 | |
166-1007B | 166-1007B-11X-4,51-53 | 96.71 | IC | d | 10 | 10 | 10 | 70 | <1 | palygorskite | 0.29 | |
166-1007C | 166-1007C-18R-3,32-35 | 468.44 | IVA | i | 95 | 5 | palygorskite | |||||
166-1007C | 166-1007C-18R-3,49-51 | 468.61 | IVA | i | <1 | 100 | palygorskite | |||||
166-1007C | 166-1007C-27R-5,46-49 | 557.56 | IVB | k | 5 | 95 | palygorskite | |||||
166-1007C | 166-1007C-31R-5,29-32 | 595.23 | IVB | k | 100 | palygorskite | ||||||
166-1007C | 166-1007C-36R-1,5-10 | 638.75 | IVB | I | 100 | palygorskite | ||||||
166-1007C | 166-1007C-43R-3,55-58 | 709.47 | V | m | ||||||||
166-1007C | 166-1007C-47R-2,29-34 | 745.99 | V | m | 100 | |||||||
166-1007C | 166-1007C-47R-2,41-42 | 746.11 | V | m | 100 | |||||||
166-1007C | 166-1007C-51R-3,118-121 | 787.16 | V | m | <1 | 100 | ||||||
166-1007C | 166-1007C-56R-2,89-91 | 833.26 | VIA | n | 5 | 95 | + | |||||
166-1007C | 166-1007C-60R-2,70-75 | 871.33 | VIA | n | <1 | 100 | ||||||
166-1007C | 166-1007C-60R-2,83-85 | 871.46 | VIA | n | 5 | 95 | + | |||||
166-1007C | 166-1007C-69R-2,12-14 | 957.54 | VIB | o | 5 | 95 | ||||||
166-1007C | 166-1007C-70R-3,75-80 | 969.20 | VIB | p | <1 | 100 | ||||||
166-1007C | 166-1007C-74R-3,104-107 | 1007.63 | VII | p | 5 | 95 | ||||||
166-1007C | 166-1007C-78R-2,14-16 | 1044.44 | VII | p2 | 100 | |||||||
166-1007C | 166-1007C-80R-3,16-18 | 1065.05 | VII | p2 | 5 | 95 | ||||||
166-1007C | 166-1007C-81R-6,22-24 | 1078.87 | VII | p2 | 5 | 95 | ||||||
166-1007C | 166-1007C-83R-3,37-40 | 1094.08 | VII | p2 | 5 | 95 | ++ | |||||
166-1007C | 166-1007C-84R-3,137-139 | 1104.54 | VII | p2 | 100 | |||||||
166-1007C | 166-1007C-84R-4,10-14 | 1104.75 | VII | p2 | 5 | 95 | <1 | +++++ | ||||
166-1007C | 166-1007C-85R-4,74-79 | 1114.22 | VII | p2 | 5 | 95 | ++++ | |||||
166-1007C | 166-1007C-91R-3,75-79 | 1171.87 | VII | q | 5 | 95 | +++ | |||||
166-1007C | 166-1007C-92R-4,69-72 | 1182.72 | VII | q | 5 | 95 | ++ | |||||
166-1007C | 166-1007C-92R-4,145-150 | 1183.48 | VII | q | 5 | 95 | + | |||||
166-1007C | 166-1007C-93R-1,75-78 | 1188.05 | VIII | q | 5 | 95 | ++ | |||||
166-1007C | 166-1007C-93R-1,129-133 | 1188.59 | VIII | q | 5 | 95 | ++ | |||||
166-1007C | 166-1007C-94R-1,22-27 | 1197.12 | VIII | r | 5 | 95 | ++ | |||||
166-1007C | 166-1007C-95R-1,66-70 | 1207.16 | VIII | r | 5 | 95 | +++ | |||||
166-1007C | 166-1007C-95R-cc,1-4 | 1208.70 | VIII | r | 5 | 95 | + |