Tribble, Jane S; Wilkens, Roy H; Arvidson, Rolf S; Busing, Christopher J (1993): (Table 2) Mineralogy of the clay size fraction of ODP Site 136-842 sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.804631, In supplement to: Tribble, JS et al. (1993): Sediments of the Hawaiian Arch: X-ray mineralogy and microfabric. In: Wilkens, RH; Firth, J; Bender, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 136, 65-76, https://doi.org/10.2973/odp.proc.sr.136.205.1993
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 19.336000 * Longitude: -159.088000
Date/Time Start: 1991-03-03T11:15:00 * Date/Time End: 1991-03-05T20:00:00
Minimum DEPTH, sediment/rock: 0.35 m * Maximum DEPTH, sediment/rock: 29.40 m
Event(s):
136-842A * Latitude: 19.336000 * Longitude: -159.088000 * Date/Time Start: 1991-03-03T11:15:00 * Date/Time End: 1991-03-04T00:30:00 * Elevation: -4441.0 m * Penetration: 9.5 m * Recovery: 9.66 m * Location: North Pacific Ocean * Campaign: Leg136 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 1 core; 9.5 m cored; 0 m drilled; 101.7 % recovery
136-842B * Latitude: 19.336000 * Longitude: -159.088000 * Date/Time Start: 1991-03-05T00:30:00 * Date/Time End: 1991-03-05T20:00:00 * Elevation: -4441.0 m * Penetration: 167.8 m * Recovery: 35.65 m * Location: North Pacific Ocean * Campaign: Leg136 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 72.3 m cored; 0 m drilled; 49.3 % recovery
Comment:
Sediment depth is given in mbsf. Abundances: ++ = abundant, + minor component, - = absent.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Tribble, Jane S | DSDP/ODP/IODP sample designation | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 4 | Smectite | Sme | % | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | |
| 5 | Illite | Ill | % | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | |
| 6 | Kaolinite+Chlorite | Kln+Chl | % | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | |
| 7 | Quartz | Qz | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | ||
| 8 | Plagioclase | Pl | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | ||
| 9 | Phillipsite | Php | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | ||
| 10 | Clinoptilolite | Cpt | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | ||
| 11 | Amorphous phase | Amorph | Tribble, Jane S | X-ray diffraction TEXTUR, clay fraction | refers to biogenic silica and/or volcanic glass |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
234 data points
Data
| 1 Event | 2 Sample label | 3 Depth sed [m] | 4 Sme [%] | 5 Ill [%] | 6 Kln+Chl [%] | 7 Qz | 8 Pl | 9 Php | 10 Cpt | 11 Amorph |
|---|---|---|---|---|---|---|---|---|---|---|
| 136-842A | 136-842A-1H-1,35 | 0.35 | 6 | 76 | 18 | ++ | ++ | - | - | - |
| 136-842A | 136-842A-1H-3,110 | 4.10 | 13 | 72 | 15 | ++ | + | - | - | + |
| 136-842A | 136-842A-1H-4,110 | 5.60 | 26 | 66 | 8 | ++ | + | - | - | + |
| 136-842A | 136-842A-1H-5,35 | 6.35 | 48 | 44 | 8 | ++ | + | - | - | + |
| 136-842A | 136-842A-1H-6,35 | 7.85 | 35 | 56 | 10 | ++ | ++ | - | - | + |
| 136-842A | 136-842A-1H-6,109 | 8.59 | 44 | 48 | 8 | ++ | ++ | - | - | - |
| 136-842A | 136-842A-1H-7,25 | 9.25 | 22 | 63 | 15 | ++ | ++ | - | - | + |
| 136-842B | 136-842B-1H-2,110 | 2.60 | 46 | 43 | 11 | + | + | - | - | + |
| 136-842B | 136-842B-1H-3,35 | 3.35 | 10 | 76 | 13 | ++ | + | - | - | + |
| 136-842B | 136-842B-1H-4,35 | 4.85 | 39 | 51 | 10 | ++ | + | - | - | + |
| 136-842B | 136-842B-1H-5,13 | 6.13 | 25 | 59 | 16 | ++ | + | - | - | + |
| 136-842B | 136-842B-2H-1,110 | 7.40 | 29 | 55 | 16 | ++ | ++ | + | - | - |
| 136-842B | 136-842B-2H-2,35 | 8.15 | 42 | 50 | 9 | ++ | + | - | - | - |
| 136-842B | 136-842B-2H-2,110 | 8.90 | 56 | 35 | 9 | ++ | + | - | - | - |
| 136-842B | 136-842B-2H-4,35 | 11.15 | 41 | 34 | 26 | + | + | ++ | - | - |
| 136-842B | 136-842B-2H-4,110 | 11.90 | 26 | 39 | 35 | + | + | ++ | - | - |
| 136-842B | 136-842B-2H-6,11 | 13.91 | 37 | 24 | 39 | + | - | ++ | - | - |
| 136-842B | 136-842B-3H-1,35 | 16.15 | 75 | 13 | 12 | + | + | + | - | - |
| 136-842B | 136-842B-3H-1,110 | 16.90 | 64 | 24 | 12 | + | + | + | - | - |
| 136-842B | 136-842B-3H-3,35 | 19.15 | 33 | 56 | 11 | ++ | + | - | - | - |
| 136-842B | 136-842B-3H-3,110 | 19.90 | 41 | 49 | 10 | + | - | - | + | - |
| 136-842B | 136-842B-3H-4,110 | 21.40 | 32 | 59 | 10 | ++ | - | - | + | - |
| 136-842B | 136-842B-3H-6,35 | 23.65 | 43 | 50 | 7 | ++ | + | - | + | - |
| 136-842B | 136-842B-3H-7,49 | 25.29 | 78 | 19 | 3 | + | - | - | + | - |
| 136-842B | 136-842B-4H-1,110 | 26.40 | 70 | 25 | 4 | ++ | + | - | + | - |
| 136-842B | 136-842B-4H-3,110 | 29.40 | 93 | 5 | 1 | + | + | - | + | - |