Cremer, Michel; Maillet, Noelle; Latouche, Claude (1989): (Table 1) Mineralogy of ODP Site 105-646 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.745577, In supplement to: Cremer, M et al. (1989): Analysis of sedimentary facies and clay mineralogy of the Neogene-Quaternary sediments in ODP Site 646, Labrador Sea. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 71-81, https://doi.org/10.2973/odp.proc.sr.105.114.1989
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 58.209300 * Longitude: -48.369100
Date/Time Start: 1985-10-03T05:45:00 * Date/Time End: 1985-10-13T21:01:00
Minimum DEPTH, sediment/rock: 4.6 m * Maximum DEPTH, sediment/rock: 758.2 m
Event(s):
105-646A * Latitude: 58.209300 * Longitude: -48.369100 * Date/Time Start: 1985-10-03T05:45:00 * Date/Time End: 1985-10-04T05:30:00 * Elevation: -3460.0 m * Penetration: 103.5 m * Recovery: 92.14 m * Location: Labrador Sea * Campaign: Leg105 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 core; 103.5 m cored; 0 m drilled; 89 % recovery
105-646B * Latitude: 58.209300 * Longitude: -48.369100 * Date/Time Start: 1985-10-04T08:45:00 * Date/Time End: 1985-10-13T21:01:00 * Elevation: -3459.0 m * Penetration: 766.7 m * Recovery: 404.25 m * Location: Labrador Sea * Campaign: Leg105 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 80 cores; 766.2 m cored; 0 m drilled; 52.8 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Sample code/label | Sample label | Cremer, Michel | DSDP/ODP/IODP sample designation | ||
3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
4 | Calcite | Cal | % | Cremer, Michel | X-ray diffraction (XRD) | bulk sediment |
5 | Quartz | Qz | % | Cremer, Michel | X-ray diffraction (XRD) | bulk sediment |
6 | Feldspar | Fsp | % | Cremer, Michel | X-ray diffraction (XRD) | bulk sediment |
7 | Chlorite | Chl | % | Cremer, Michel | X-ray diffraction (XRD) | |
8 | Illite | Ill | % | Cremer, Michel | X-ray diffraction (XRD) | |
9 | Clay minerals | Clay min | Cremer, Michel | X-ray diffraction (XRD) | interlayerd clay minerals, T = trace, P = present, - = absent | |
10 | Smectite | Sme | % | Cremer, Michel | X-ray diffraction (XRD) | |
11 | Kaolinite | Kln | % | Cremer, Michel | X-ray diffraction (XRD) | < 1 = trace |
12 | Quartz | Qz | Cremer, Michel | X-ray diffraction (XRD) | T = trace, P = present, - = absent | |
13 | Feldspar | Fsp | Cremer, Michel | X-ray diffraction (XRD) | T = trace, P = present, - = absent | |
14 | Amphibole | Amp | Cremer, Michel | X-ray diffraction (XRD) | T = trace, P = present, - = absent |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
648 data points
Data
1 Event | 2 Sample label | 3 Depth sed [m] | 4 Cal [%] | 5 Qz [%] | 6 Fsp [%] | 7 Chl [%] | 8 Ill [%] | 9 Clay min | 10 Sme [%] | 11 Kln [%] | 12 Qz | 13 Fsp | 14 Amp |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
105-646A | 105-646A-1H-4,7-12 | 4.6 | 3 | 7 | 20 | 35 | 29 | T | 36 | <1 | T | P | T |
105-646A | 105-646A-3H-3,33-38 | 19.8 | 5 | 14 | 38 | 29 | 36 | T | 29 | 6 | T | P | P |
105-646A | 105-646A-4H-3,5-10 | 29.2 | 40 | 4 | 15 | 16 | 32 | T | 44 | 8 | T | P | T |
105-646A | 105-646A-5H-3,10-15 | 38.9 | 9 | 12 | 23 | 29 | 36 | - | 26 | 9 | T | P | - |
105-646A | 105-646A-6H-3,82-87 | 48.3 | 4 | 10 | 30 | 24 | 32 | - | 32 | 12 | T | P | P |
105-646A | 105-646A-7H-4,57-61 | 60.2 | 3 | 10 | 23 | 21 | 29 | - | 32 | 18 | - | P | P |
105-646A | 105-646A-8H-1,107-111 | 65.9 | <1 | 10 | 26 | 24 | 29 | T | 35 | 12 | T | P | P |
105-646A | 105-646A-10H-3,63-68 | 87.7 | 2 | 8 | 50 | 21 | 21 | P | 44 | 14 | T | P | T |
105-646A | 105-646A-11H-4,36-41 | 98.6 | 4 | 10 | 30 | 26 | 32 | T | 29 | 13 | - | P | P |
105-646B | 105-646B-12H-6,9-14 | 109.0 | 1 | 9 | 25 | 24 | 29 | T | 37 | 10 | T | P | P |
105-646B | 105-646B-13H-2,84-89 | 113.4 | 0 | 14 | 23 | 22 | 39 | T | 28 | 11 | T | P | P |
105-646B | 105-646B-18X-2,84-89 | 161.4 | 10 | 10 | 48 | 22 | 26 | T | 43 | 9 | T | P | T |
105-646B | 105-646B-20X-3,7-13 | 181.6 | 0 | 16 | 40 | 18 | 29 | - | 41 | 12 | T | P | T |
105-646B | 105-646B-22X-1,34-36 | 198.1 | 0 | 20 | 30 | 22 | 28 | T | 39 | 11 | T | P | T |
105-646B | 105-646B-22X-4,40-42 | 202.7 | 0 | 20 | 48 | 20 | 33 | T | 40 | 7 | T | P | T |
105-646B | 105-646B-23X-1,93-95 | 208.4 | 0 | 16 | 27 | 14 | 24 | T | 52 | 10 | T | P | T |
105-646B | 105-646B-23X-4,92-94 | 212.9 | 0 | 18 | 38 | 18 | 33 | T | 40 | 9 | T | P | T |
105-646B | 105-646B-26X-2,60-65 | 238.2 | 4 | 10 | 26 | 22 | 28 | P | 37 | 13 | T | P | P |
105-646B | 105-646B-29X-1,90-95 | 266.2 | 0 | 12 | 38 | 27 | 37 | - | 23 | 13 | T | P | T |
105-646B | 105-646B-30X-4,65-70 | 280.2 | 0 | 8 | 36 | 27 | 37 | - | 27 | 9 | P | P | T |
105-646B | 105-646B-31X-3,109-114 | 288.8 | 10 | 16 | 36 | 20 | 32 | T | 40 | 8 | T | P | T |
105-646B | 105-646B-32X-4,71-76 | 299.0 | 26 | 14 | 26 | 21 | 36 | T | 29 | 14 | T | P | T |
105-646B | 105-646B-33X-2,112-117 | 306.7 | 5 | 8 | 26 | 19 | 28 | T | 39 | 14 | T | P | T |
105-646B | 105-646B-35X-1,38-40 | 323.8 | 0 | 10 | 26 | 24 | 40 | - | 22 | 14 | T | P | T |
105-646B | 105-646B-36X-4,97-99 | 338.6 | 0 | 10 | 26 | 15 | 31 | T | 39 | 15 | T | P | T |
105-646B | 105-646B-36X-6,102-104 | 341.6 | 8 | 8 | 23 | 15 | 20 | P | 55 | 10 | T | T | P |
105-646B | 105-646B-37X-4,62-67 | 347.9 | 2 | 10 | 36 | 19 | 23 | P | 50 | 8 | T | P | T |
105-646B | 105-646B-40X-2,97-102 | 374.2 | 6 | 10 | 30 | 35 | 33 | T | 33 | 9 | T | P | P |
105-646B | 105-646B-41X-3,65-68 | 385.0 | 11 | 10 | 23 | 26 | 36 | T | 21 | 17 | T | P | P |
105-646B | 105-646B-42X-3,102-107 | 395.0 | 2 | 15 | 56 | 22 | 33 | T | 33 | 12 | T | P | P |
105-646B | 105-646B-43X-2,25-27 | 402.5 | 4 | 10 | 30 | 20 | 30 | T | 40 | 10 | T | P | P |
105-646B | 105-646B-49X-2,81-85 | 461.1 | 21 | 8 | 20 | 13 | 32 | T | 45 | 10 | T | P | P |
105-646B | 105-646B-50X-3,34-39 | 471.8 | 18 | 10 | 16 | 30 | 32 | T | 28 | 10 | P | P | P |
105-646B | 105-646B-51X-2,2-7 | 479.6 | 0 | 10 | 26 | 17 | 40 | T | 30 | 13 | T | P | T |
105-646B | 105-646B-56X-1,83-85 | 527.5 | 0 | 8 | 26 | 21 | 37 | T | 26 | 16 | T | P | T |
105-646B | 105-646B-58X-2,55-58 | 547.5 | 0 | 11 | 26 | 19 | 25 | - | 47 | 9 | T | P | P |
105-646B | 105-646B-60X-3,42-45 | 567.8 | 17 | 11 | 23 | 18 | 46 | P | 27 | 9 | T | P | T |
105-646B | 105-646B-61X-1,134-136 | 575.3 | 0 | 14 | 40 | 19 | 36 | - | 32 | 13 | T | P | T |
105-646B | 105-646B-62X-2,10-12 | 585.2 | 14 | 10 | 20 | 21 | 38 | T | 31 | 10 | T | P | T |
105-646B | 105-646B-62X-3,60-62 | 587.2 | 13 | 7 | 23 | 17 | 35 | T | 35 | 13 | T | P | T |
105-646B | 105-646B-63X-1,126-128 | 594.5 | 6 | 10 | 26 | 16 | 36 | T | 36 | 12 | T | P | P |
105-646B | 105-646B-65X-4,45-49 | 617.5 | 6 | 12 | 23 | 18 | 31 | P | 42 | 9 | P | P | T |
105-646B | 105-646B-66X-1,86-89 | 623.1 | 15 | 18 | 32 | 19 | 40 | T | 32 | 9 | T | P | T |
105-646B | 105-646B-67X-3,86-89 | 635.7 | 4 | 19 | 30 | 18 | 33 | T | 42 | 7 | T | P | T |
105-646B | 105-646B-68X-2,122-127 | 644.0 | 0 | 14 | 22 | 16 | 37 | T | 37 | 10 | P | T | - |
105-646B | 105-646B-69X-1,99-102 | 651.9 | 15 | 11 | 18 | 16 | 31 | T | 45 | 8 | T | P | P |
105-646B | 105-646B-71X-2,91-93 | 672.6 | 2 | 10 | 20 | 22 | 29 | T | 42 | 7 | P | P | T |
105-646B | 105-646B-72X-1,123-125 | 680.9 | 11 | 14 | 14 | 17 | 32 | - | 42 | 9 | T | P | P |
105-646B | 105-646B-74X-2,46-50 | 701.0 | 8 | 10 | 14 | 13 | 28 | T | 49 | 10 | T | P | T |
105-646B | 105-646B-75X-4,77-80 | 712.9 | 0 | 14 | 15 | 14 | 26 | - | 53 | 7 | T | P | T |
105-646B | 105-646B-76X-2,64-67 | 720.4 | 0 | 14 | 20 | 12 | 23 | T | 59 | 6 | T | T | T |
105-646B | 105-646B-77X-4,54-56 | 731.9 | 0 | 18 | 23 | 9 | 22 | T | 63 | 6 | T | P | T |
105-646B | 105-646B-78X-2,125-127 | 739.5 | 0 | 14 | 23 | 16 | 22 | P | 53 | 9 | T | P | T |
105-646B | 105-646B-80X-1,125-127 | 758.2 | 4 | 10 | 26 | 15 | 23 | T | 56 | 6 | T | P | T |