Lackschewitz, Klas Sven; Singer, A; Botz, Reiner; Garbe-Schönberg, Dieter; Stoffers, Peter (2000): (Table T2) Mineralogy of unaltered, altered, and strongly altered sediments from ODP Site 169-1038 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.788706, In supplement to: Lackschewitz, KS et al. (2000): Mineralogy and geochemistry of clay minerals near a hydrothermal site in the Escanaba Trough, Gorda Ridge, northeast Pacific Ocean. In: Zierenberg, RA; Fouquet, Y; Miller, DJ; Normark, WR (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 169, 1-24, https://doi.org/10.2973/odp.proc.sr.169.116.2000
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 40.997837 * Median Longitude: -127.491663 * South-bound Latitude: 40.995410 * West-bound Longitude: -127.494190 * North-bound Latitude: 41.000080 * East-bound Longitude: -127.488080
Date/Time Start: 1996-10-07T00:15:00 * Date/Time End: 1996-10-09T15:30:00
Minimum DEPTH, sediment/rock: 3.90 m * Maximum DEPTH, sediment/rock: 387.54 m
Event(s):
169-1038G * Latitude: 40.995410 * Longitude: -127.488080 * Date/Time: 1996-10-07T00:15:00 * Elevation: -3239.2 m * Penetration: 147 m * Recovery: 44.88 m * Location: Escanaba Trough, North Pacific Ocean * Campaign: Leg169 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 147 m cored; 0 m drilled; 30.5 % recovery
169-1038H * Latitude: 41.000080 * Longitude: -127.494190 * Date/Time: 1996-10-08T10:00:00 * Elevation: -3222.2 m * Penetration: 192.8 m * Recovery: 30 m * Location: Escanaba Trough, North Pacific Ocean * Campaign: Leg169 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 192.8 m cored; 0 m drilled; 15.6 % recovery
169-1038I * Latitude: 40.998020 * Longitude: -127.492720 * Date/Time: 1996-10-09T15:30:00 * Elevation: -3215.2 m * Penetration: 404 m * Recovery: 191.13 m * Location: Escanaba Trough, North Pacific Ocean * Campaign: Leg169 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 404 m cored; 0 m drilled; 47.3 % recovery
Comment:
Sediment depth is given in mbsf. Mineral occurrence was defined as follows: V = very abundant, A = abundant, C = common, R = rare, Tr = trace, - = absent.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Lackschewitz, Klas Sven | DSDP/ODP/IODP sample designation | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 4 | Lithologic unit/sequence | Unit | Lackschewitz, Klas Sven | |||
| 5 | Quartz | Qz | Lackschewitz, Klas Sven | X-ray diffraction (XRD) | ||
| 6 | Feldspar | Fsp | Lackschewitz, Klas Sven | X-ray diffraction (XRD) | ||
| 7 | Pyroxene | Pyrox | Lackschewitz, Klas Sven | X-ray diffraction (XRD) | ||
| 8 | Illite | Ill | Lackschewitz, Klas Sven | X-ray diffraction (XRD) | ||
| 9 | Smectite | Sme | Lackschewitz, Klas Sven | X-ray diffraction (XRD) | ||
| 10 | Chlorite-smectite | Chl-Sme | Lackschewitz, Klas Sven | X-ray diffraction (XRD) | mixed layer; (% of chlorite layers in Chl-smec) | |
| 11 | Chlorite | Chl | Lackschewitz, Klas Sven | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
252 data points
Data
| 1 Event | 2 Sample label | 3 Depth sed [m] | 4 Unit | 5 Qz | 6 Fsp | 7 Pyrox | 8 Ill | 9 Sme | 10 Chl-Sme | 11 Chl |
|---|---|---|---|---|---|---|---|---|---|---|
| 169-1038G | 169-1038G-3H-3,128-138 | 25.08 | II | A | R | Tr | R | - | R (30) | C |
| 169-1038G | 169-1038G-4H-2,99-101 | 33.99 | II | C | Tr | Tr | R | - | - | A |
| 169-1038G | 169-1038G-4H-6,4-6 | 37.76 | II | C | R | Tr | R | - | - | A |
| 169-1038G | 169-1038G-5H-6,71-73 | 48.08 | II | C | Tr | Tr | R | - | - | A |
| 169-1038G | 169-1038G-6X-3,12-14 | 53.62 | II | C | R | Tr | R | - | - | A |
| 169-1038G | 169-1038G-7X-1,125-127 | 61.75 | II | C | R | Tr | R | - | - | C |
| 169-1038G | 169-1038G-8X-CC,22-24 | 70.89 | III | R | Tr | Tr | R | - | - | A |
| 169-1038G | 169-1038G-10X-1,38-40 | 89.68 | III | C | R | Tr | R | - | - | A |
| 169-1038G | 169-1038G-11X-CC,8-10 | 98.98 | III | C | R | Tr | C | - | R (20) | A |
| 169-1038G | 169-1038G-13X-CC,4-6 | 118.24 | III | C | Tr | Tr | C | - | R (20) | R |
| 169-1038H | 169-1038H-1X-3,90-92 | 3.90 | II | C | - | - | Tr | - | - | A |
| 169-1038H | 169-1038H-2X-2,43-45 | 13.83 | II | Tr | - | - | Tr | - | - | V |
| 169-1038H | 169-1038H-3X-1,34-36 | 21.84 | II | C | - | - | Tr | - | - | A |
| 169-1038H | 169-1038H-4X-2,6-8 | 31.06 | II | R | R | Tr | R | - | - | A |
| 169-1038H | 169-1038H-5X-4,5-7 | 43.65 | II | C | R | Tr | R | - | - | C |
| 169-1038H | 169-1038H-6X-1,42-44 | 49.12 | II | C | R | Tr | R | - | - | A |
| 169-1038H | 169-1038H-14X-CC,25-28 | 126.15 | IV? | C | R | Tr | R | - | - | A |
| 169-1038H | 169-1038H-20X-CC,23-25 | 183.83 | VI? | C | C | Tr | R | - | - | C |
| 169-1038I | 169-1038I-1X-3,99-101 | 3.99 | II | C | R | Tr | R | - | - | C |
| 169-1038I | 169-1038I-2X-1,53-55 | 9.83 | II | C | R | Tr | R | - | - | C |
| 169-1038I | 169-1038I-4H-6,83-85 | 35.21 | II | C | R | Tr | R | - | - | C |
| 169-1038I | 169-1038I-7H-1,136-138 | 56.66 | II | C | R | Tr | R | - | - | C |
| 169-1038I | 169-1038I-8X-2,130-132 | 67.60 | II | C | R | Tr | R | - | - | C |
| 169-1038I | 169-1038I-17X-1,104-106 | 152.34 | IV | C | R | Tr | R | - | - | C |
| 169-1038I | 169-1038I-20X-1,84-85 | 180.94 | VI | C | Tr | Tr | Tr | - | - | C |
| 169-1038I | 169-1038I-23X-1,6-8 | 209.06 | VI | C | Tr | Tr | Tr | - | Tr (10, 80) | C |
| 169-1038I | 169-1038I-28X-4,125-127 | 262.85 | VI | C | Tr | Tr | Tr | - | Tr (20) | C |
| 169-1038I | 169-1038I-41X-4,94-96 | 387.54 | VIII | C | Tr | Tr | Tr | Tr | Tr (50) | C |