Clayton, T; Kemp, Alan E S (1990): (Table 1) Clay-mineral composition of ODP Site 112-679 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.753098, In supplement to: Clayton, T; Kemp, AES (1990): Clay mineralogy of Cenozoic Sediments from the Peruvian continental margin: Leg 112. In: Suess, E; von Huene, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 112, 59-86, https://doi.org/10.2973/odp.proc.sr.112.137.1990
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -11.063415 * Median Longitude: -78.272250 * South-bound Latitude: -11.063830 * West-bound Longitude: -78.272330 * North-bound Latitude: -11.063000 * East-bound Longitude: -78.272170
Date/Time Start: 1986-11-01T12:45:00 * Date/Time End: 1986-11-05T03:15:00
Minimum Elevation: -462.0 m * Maximum Elevation: -462.0 m
Event(s):
112-679D * Latitude: -11.063830 * Longitude: -78.272170 * Date/Time Start: 1986-11-01T12:45:00 * Date/Time End: 1986-11-02T13:15:00 * Elevation: -462.0 m * Penetration: 245.4 m * Recovery: 116.03 m * Location: South Pacific Ocean * Campaign: Leg112 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 27 cores; 245.2 m cored; 0 m drilled; 47.3 % recovery
112-679E * Latitude: -11.063000 * Longitude: -78.272330 * Date/Time Start: 1986-11-02T13:15:00 * Date/Time End: 1986-11-05T03:15:00 * Elevation: -462.0 m * Penetration: 359.3 m * Recovery: 36.3 m * Location: South Pacific Ocean * Campaign: Leg112 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 114 m cored; 0 m drilled; 31.8 % recovery
Comment:
+ = present, - = absent
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Clayton, T | DSDP/ODP/IODP sample designation | ||
| 3 | Palygorskite | Plg | % | Clayton, T | X-ray diffraction, clay fraction | |
| 4 | Clay minerals | Clay min | % | Clayton, T | X-ray diffraction, clay fraction | expandable |
| 5 | Illite | Ill | % | Clayton, T | X-ray diffraction, clay fraction | |
| 6 | Chlorite | Chl | % | Clayton, T | X-ray diffraction, clay fraction | |
| 7 | Kaolinite | Kln | % | Clayton, T | X-ray diffraction, clay fraction | |
| 8 | Chlorite-smectite | Chl-Sme | Clayton, T | X-ray diffraction, clay fraction | ||
| 9 | Clinoptilolite | Cpt | Clayton, T | X-ray diffraction, clay fraction | ||
| 10 | - | - | Clayton, T | X-ray diffraction, clay fraction | d(001) (A) of expanding phase |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
288 data points
Data
| 1 Event | 2 Sample label | 3 Plg [%] | 4 Clay min [%] | 5 Ill [%] | 6 Chl [%] | 7 Kln [%] | 8 Chl-Sme | 9 Cpt | 10 - |
|---|---|---|---|---|---|---|---|---|---|
| 112-679D | 112-679D-1H-1,106-108 | 0 | 39 | 44 | 11 | 6 | - | - | 16.2 |
| 112-679D | 112-679D-2H-1,120-122 | 0 | 47 | 40 | 8 | 5 | + | - | 16.2 |
| 112-679D | 112-679D-3H-1,44-46 | 0 | 45 | 45 | 7 | 3 | + | - | 15.5 |
| 112-679D | 112-679D-5H-1,16-18 | 0 | 47 | 42 | 7 | 4 | + | - | 15.8 |
| 112-679D | 112-679D-6H-1,86-88 | 0 | 65 | 26 | 5 | 4 | - | - | 16.2 |
| 112-679D | 112-679D-7H-1,46-48 | 0 | 65 | 26 | 5 | 4 | - | - | 16.7 |
| 112-679D | 112-679D-8H-1,88-90 | 0 | 59 | 31 | 7 | 3 | - | - | 15.8 |
| 112-679D | 112-679D-9H-1,111-113 | 0 | 64 | 26 | 6 | 4 | + | - | 16.4 |
| 112-679D | 112-679D-10H-1,68-70 | 0 | 66 | 24 | 6 | 4 | + | - | 16.1 |
| 112-679D | 112-679D-11H-1,44-46 | 0 | 73 | 18 | 6 | 3 | + | - | 16.8 |
| 112-679D | 112-679D-13X-1,33-35 | 0 | 74 | 20 | 3 | 3 | + | - | 16.2 |
| 112-679D | 112-679D-14X-1,36-38 | 0 | 74 | 20 | 4 | 2 | + | - | 16.7 |
| 112-679D | 112-679D-15X-1,34-36 | 0 | 67 | 21 | 8 | 4 | + | - | 16.8 |
| 112-679D | 112-679D-17X-1,104-106 | 0 | 85 | 11 | 3 | 1 | + | - | 16.7 |
| 112-679D | 112-679D-18X-1,120-122 | 0 | 75 | 16 | 6 | 3 | + | - | 17.0 |
| 112-679D | 112-679D-19X-1,65-67 | 0 | 82 | 14 | 2 | 2 | + | - | 16.8 |
| 112-679D | 112-679D-20X-1,69-71 | 0 | 75 | 17 | 5 | 3 | + | - | 17.0 |
| 112-679D | 112-679D-21X-CC,7-9 | 0 | 82 | 12 | 4 | 2 | + | - | 17.0 |
| 112-679D | 112-679D-22X-CC,9-11 | 0 | 79 | 15 | 4 | 2 | + | + | 17.0 |
| 112-679D | 112-679D-23X-CC,5-7 | 0 | 74 | 18 | 5 | 3 | + | - | 16.8 |
| 112-679D | 112-679D-24X-1,22-24 | 0 | 77 | 17 | 4 | 2 | + | + | 16.8 |
| 112-679D | 112-679D-26X-1,44-46 | 0 | 82 | 14 | 3 | 1 | - | + | 16.8 |
| 112-679E | 112-679E-3X-1,50-52 | 0 | 94 | 4 | 1 | 1 | - | + | 17.0 |
| 112-679E | 112-679E-4X-1,23-25 | 0 | 91 | 7 | 1 | 1 | - | + | 17.0 |
| 112-679E | 112-679E-5X-1,84-86 | 0 | 91 | 7 | 1 | 1 | - | + | 16.8 |
| 112-679E | 112-679E-6X-1,67-69 | 0 | 81 | 16 | 1 | 2 | + | - | 16.8 |
| 112-679E | 112-679E-7X-1,37-39 | 0 | 84 | 13 | 1 | 2 | - | + | 17.0 |
| 112-679E | 112-679E-8X-1,20-22 | 0 | 92 | 6 | 1 | 1 | - | + | 17.0 |
| 112-679E | 112-679E-9X-1,40-42 | 0 | 89 | 8 | 1 | 2 | + | + | 17.0 |
| 112-679E | 112-679E-10X-1,43-45 | 0 | 84 | 12 | 2 | 2 | + | + | 17.0 |
| 112-679E | 112-679E-11X-1,51-53 | 0 | 84 | 11 | 3 | 2 | - | - | 17.0 |
| 112-679E | 112-679E-12X-1,54-56 | 0 | 91 | 7 | 1 | 1 | + | - | 17.0 |