Clayton, T; Kemp, Alan E S (1990): (Table 5) Clay-mineral composition of ODP Site 112-683 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.753102, 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: -9.027335 * Median Longitude: -80.405500 * South-bound Latitude: -9.028170 * West-bound Longitude: -80.406670 * North-bound Latitude: -9.026500 * East-bound Longitude: -80.404330
Date/Time Start: 1986-11-15T07:22:00 * Date/Time End: 1986-11-20T18:00:00
Minimum Elevation: -3087.0 m * Maximum Elevation: -3077.0 m
Event(s):
112-683A * Latitude: -9.028170 * Longitude: -80.406670 * Date/Time Start: 1986-11-15T07:22:00 * Date/Time End: 1986-11-18T16:30:00 * Elevation: -3087.0 m * Penetration: 419.2 m * Recovery: 217.67 m * Location: South Pacific Ocean * Campaign: Leg112 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 45 cores; 419.2 m cored; 0 m drilled; 51.9 % recovery
112-683B * Latitude: -9.026500 * Longitude: -80.404330 * Date/Time Start: 1986-11-18T16:30:00 * Date/Time End: 1986-11-20T18:00:00 * Elevation: -3077.0 m * Penetration: 488 m * Recovery: 30.67 m * Location: South Pacific Ocean * Campaign: Leg112 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 85.5 m cored; 0 m drilled; 35.9 % 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:
441 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 - |
|---|---|---|---|---|---|---|---|---|---|
| 112-683A | 112-683A-1H-1,86-88 | 0 | 57 | 32 | 8 | 3 | + | - | 16.5 |
| 112-683A | 112-683A-2H-1,86-88 | 0 | 37 | 45 | 12 | 6 | - | - | 16.8 |
| 112-683A | 112-683A-3H-1,86-88 | 0 | 54 | 34 | 9 | 3 | - | - | 16.1 |
| 112-683A | 112-683A-4H-1,80-82 | 0 | 42 | 46 | 8 | 4 | + | - | 16.1 |
| 112-683A | 112-683A-5H-1,80-82 | 0 | 51 | 36 | 9 | 4 | + | - | 16.5 |
| 112-683A | 112-683A-6H-1,84-86 | 0 | 40 | 46 | 7 | 7 | + | - | 16.1 |
| 112-683A | 112-683A-7H-1,84-86 | 0 | 43 | 42 | 10 | 5 | - | - | 16.1 |
| 112-683A | 112-683A-8H-1,84-86 | 0 | 43 | 43 | 9 | 5 | - | - | 15.8 |
| 112-683A | 112-683A-10X-1,82-84 | 0 | 33 | 55 | 10 | 2 | + | - | 14.2 |
| 112-683A | 112-683A-11X-1,79-81 | 0 | 34 | 54 | 8 | 4 | - | - | 14.4 |
| 112-683A | 112-683A-12X-1,73-75 | 0 | 38 | 47 | 10 | 5 | + | - | 14.5 |
| 112-683A | 112-683A-13X-1,73-75 | 0 | 33 | 53 | 10 | 4 | - | - | 15.2 |
| 112-683A | 112-683A-14X-1,73-75 | 0 | 32 | 52 | 12 | 4 | - | - | 15.0 |
| 112-683A | 112-683A-15X-1,73-75 | 0 | 39 | 48 | 9 | 4 | - | - | 15.0 |
| 112-683A | 112-683A-16X-1,27-29 | 0 | 33 | 49 | 12 | 6 | - | - | 15.5 |
| 112-683A | 112-683A-18X-1,27-29 | 0 | 31 | 54 | 10 | 5 | - | - | 14.2 |
| 112-683A | 112-683A-19X-1,34-36 | 0 | 39 | 47 | 11 | 3 | - | - | 14.2 |
| 112-683A | 112-683A-21X-1,34-36 | 0 | 33 | 54 | 9 | 4 | - | - | 14.2 |
| 112-683A | 112-683A-22X-1,39-41 | 0 | 42 | 45 | 8 | 5 | - | - | 14.2 |
| 112-683A | 112-683A-23X-1,39-41 | 0 | 41 | 44 | 10 | 5 | - | - | 15.8 |
| 112-683A | 112-683A-24X-1,49-51 | 0 | 53 | 36 | 8 | 3 | - | - | 15.5 |
| 112-683A | 112-683A-26X-1,37-39 | 0 | 58 | 32 | 6 | 4 | - | - | 15.9 |
| 112-683A | 112-683A-27X-1,28-30 | 0 | 52 | 34 | 7 | 7 | - | - | 15.2 |
| 112-683A | 112-683A-28X-1,21-23 | 0 | 51 | 34 | 9 | 6 | - | - | 15.8 |
| 112-683A | 112-683A-29X-1,21-23 | 0 | 51 | 35 | 9 | 5 | + | - | 16.4 |
| 112-683A | 112-683A-30X-1,21-23 | 0 | 56 | 32 | 6 | 6 | + | - | 16.7 |
| 112-683A | 112-683A-31X-1,21-23 | 0 | 48 | 38 | 10 | 4 | + | - | 16.4 |
| 112-683A | 112-683A-32X-1,74-76 | 0 | 61 | 30 | 4 | 5 | - | - | 16.1 |
| 112-683A | 112-683A-33X-3,103-105 | 0 | 59 | 29 | 5 | 7 | - | - | 16.8 |
| 112-683A | 112-683A-34X-1,74-76 | 0 | 64 | 26 | 6 | 4 | - | - | 17.0 |
| 112-683A | 112-683A-35X-1,33-35 | 0 | 60 | 29 | 6 | 5 | - | - | 17.0 |
| 112-683A | 112-683A-36X-1,37-39 | 0 | 61 | 25 | 6 | 8 | - | - | 17.0 |
| 112-683A | 112-683A-37X-1,62-64 | 0 | 69 | 18 | 8 | 5 | - | - | 17.0 |
| 112-683A | 112-683A-40X-1,62-64 | 0 | 62 | 25 | 6 | 7 | - | - | 17.0 |
| 112-683A | 112-683A-41X-1,45-47 | 0 | 68 | 21 | 6 | 5 | + | - | 17.0 |
| 112-683A | 112-683A-42X-1,45-47 | 0 | 62 | 24 | 6 | 8 | - | - | 17.0 |
| 112-683A | 112-683A-43X-1,16-18 | 0 | 66 | 23 | 5 | 6 | - | - | 17.0 |
| 112-683A | 112-683A-44X-1,51-53 | 0 | 80 | 13 | 3 | 4 | - | - | 16.8 |
| 112-683A | 112-683A-45X-2,12-14 | 0 | 71 | 20 | 4 | 5 | - | - | 17.1 |
| 112-683A | 112-683A-45X-5,50-52 | 0 | 77 | 15 | 4 | 4 | - | - | 17.1 |
| 112-683B | 112-683B-1X-1,45-47 | 0 | 61 | 27 | 6 | 6 | - | - | 17.0 |
| 112-683B | 112-683B-2X-1,89-91 | 0 | 67 | 24 | 5 | 4 | - | - | 17.0 |
| 112-683B | 112-683B-3X-1,60-62 | 0 | 66 | 21 | 6 | 7 | - | - | 16.7 |
| 112-683B | 112-683B-5X-1,69-71 | 0 | 68 | 19 | 7 | 6 | - | - | 16.8 |
| 112-683B | 112-683B-5X-3,6-8 | 0 | 72 | 21 | 3 | 4 | - | - | 17.0 |
| 112-683B | 112-683B-6X-1,32-34 | 0 | 72 | 19 | 4 | 5 | - | - | 17.0 |
| 112-683B | 112-683B-6X-3,72-74 | 0 | 70 | 20 | 5 | 5 | - | - | 17.0 |
| 112-683B | 112-683B-7X-1,99-101 | 0 | 84 | 15 | 1 | 0 | - | - | 17.1 |
| 112-683B | 112-683B-7X-2,72-74 | 0 | 89 | 10 | 0 | 1 | - | - | 17.0 |