CRP Science Team (2006): Schematic summary showing the down-hole distribution of lithic sand grains in sediment core CRP-3 sanstones (Table 4.8) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.509447, In supplement to: Barrett, Peter J; Sarti, Massimo; Wise, Sherwood W (2000): Studies from the Cape Roberts Project, Ross Sea, Antarctica, Initial Reports on CRP-3. Terra Antartica, 7(1/2), 209 pp, hdl:10013/epic.28287.d001
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Project(s):
Cape Roberts Project (CRP)
Coverage:
Latitude: -77.006000 * Longitude: 163.719000
Date/Time Start: 1999-10-09T00:00:00 * Date/Time End: 1999-11-19T00:00:00
Minimum DEPTH, sediment/rock: 24.32 m * Maximum DEPTH, sediment/rock: 750.02 m
Event(s):
CRP-3 * Latitude: -77.006000 * Longitude: 163.719000 * Date/Time Start: 1999-10-09T00:00:00 * Date/Time End: 1999-11-19T00:00:00 * Elevation: -295.0 m * Penetration: 939 m * Recovery: 936 m * Location: Ross Sea * Campaign: CRP-3 * Basis: Sampling/drilling from ice * Method/Device: Core wireline system (CWS) * Comment: 11.76 km at 76° true from Cape Roberts, 2.04 km at 225° true from CRP-2. Fast ice thickness: 2.0 to 2.2 m. Sea rise embedded to 9.55 mbsf. Lateral ice movement from spudding 5.0 m to 82° true. HQ core to 345.85 mbsf. NQ core to 939.42 mbsf. Core recovery 97%. Phase 1 logging to 345 mbsf, Phase 2 logging to 773 mbsf, Phase 3 logging to 918 mbsf. Deepest Cenozoic lithology and depth: sandstone breccia from 822.87 to 823.11 mbsf. Age of oldest Cenozoic strata: earliest Oligocene or latest Eocene. Deepest core lithology and depth: light red-brown quartz-cemented quartz sandstone to 939.42 mbsf. Age of bedrock: (mid?) Devonian.
Comment:
P = present, D = dominant
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Hornblende | Hbl | CRP Science Team | |||
3 | Biotite | Bt | CRP Science Team | |||
4 | Muscovite | Ms | CRP Science Team | |||
5 | Opaque minerals | Opaque | CRP Science Team | |||
6 | Zircon | Zrn | CRP Science Team | |||
7 | Sphene | Spn | CRP Science Team | |||
8 | Garnet | Grt | CRP Science Team | |||
9 | Minerals | Minerals | CRP Science Team | |||
10 | Quartz | Qz | CRP Science Team | Quartz-mica tectonite, ribbon quartz | ||
11 | Quartz | Qz | CRP Science Team | Polycrystalline quartz, chalcedony | ||
12 | Lithic grains | Lithic | CRP Science Team | Felsic volcanic lithic grains | ||
13 | Basalt | Basalt | CRP Science Team | Basaltic volcanic lithic grains. Fine basalts with feathery texture or rod-like opaque oxide | ||
14 | Basalt | Basalt | CRP Science Team | Basaltic volcanic lithic grains. Fine basalts with lathy plagioclase | ||
15 | Dolerite | Dolerite | CRP Science Team | |||
16 | Quartz and Feldspar | Qz+Fsp | CRP Science Team | Graphic-textured quartz-feldspar | ||
17 | Granite | Granite | CRP Science Team | |||
18 | Mud clast | Mud clast | CRP Science Team | Mudstone, sandstone (micaceous) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
475 data points
Data
1 Depth sed [m] | 2 Hbl | 3 Bt | 4 Ms | 5 Opaque | 6 Zrn | 7 Spn | 8 Grt | 9 Minerals | 10 Qz (Quartz-mica tectonite, ribbon...) | 11 Qz (Polycrystalline quartz, chalc...) | 12 Lithic (Felsic volcanic lithic grains) | 13 Basalt (Basaltic volcanic lithic grai...) | 14 Basalt (Basaltic volcanic lithic grai...) | 15 Dolerite | 16 Qz+Fsp (Graphic-textured quartz-feldspar) | 17 Granite | 18 Mud clast (Mudstone, sandstone (micaceous)) |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
24.32 | P | P? | P | P | D | P | |||||||||||
67.06 | P | P | P | P | P | P | P | ||||||||||
89.50 | P | P | P | P | P | P | epidote?, bioclastic carb | P | P | P | |||||||
177.22 | P | P | P | epidote | P | P? | D | P | D | P | |||||||
183.69 | P | P | P | D | P | P | |||||||||||
202.59 | P | P | P | P | P | P | P | P? | P | D | P | ||||||
207.71 | P | P | P | P | P | detrital carbonate? | P | ||||||||||
226.42 | P? | P (in qtz) | P | P | D | P | P | P | |||||||||
235.50 | P | P | P | P | P | P | P | P | |||||||||
256.66 | P | P | P | P | P | P | P | bioclastic carbonate | P? | P | |||||||
259.28 | P | P? | P | ||||||||||||||
279.68 | P? | P | P | epidote | P | P | P | ||||||||||
286.17 | P | ? | P | P | ? | clinozoisite? | P | P | |||||||||
289.22 | P | P | P | P | P | P | P | P | P | P | P | ||||||
315.77 | P? | P | P | P | bioclastic carbonate | P | P | P | D | P | |||||||
326.67 | P | P | P | P | P | P | P | P | P | P | |||||||
335.96 | P | P | ? | P | P | P | P | P | P | ||||||||
345.76 | ? | P (in qtz) | P | P | P? | P | P | P | P | P | |||||||
348.70 | P | P | P | P | P | P | P | ||||||||||
351.88 | P | P | P | P | P | P | |||||||||||
358.95 | P | P? | P | P | P | epidote | P | P | P | P | |||||||
369.64 | P | P | epidote | P | D | P | P | P | |||||||||
375.32 | P (in qtz) | P | P | P | P | P | P | P | P | ||||||||
383.76 | P | P | P | P | P | P | P | P | |||||||||
387.46 | P | P | P | P | P | P | P | P | P | ||||||||
390.78 | P | P | P | P | P | P | |||||||||||
396.58 | P | P | P | D | P | P | |||||||||||
405.75 | P | P? | P | P | P | P | epidote | P | P | P | P | P | |||||
413.09 | P | P | P | ||||||||||||||
415.94 | P | P | P | P | P? | P | P? | P | P | ||||||||
422.81 | P | P? | P | P | P | P | P | P | |||||||||
426.77 | P | P (in qtz) | P | P | D | P | P | P | |||||||||
437.12 | P | P | P | P | P | P | P | ||||||||||
445.23 | P | P (in qtz) | P | P | P | D | D | P | P | ||||||||
449.73 | P | P | P | P? | P | P | P | ||||||||||
455.81 | P | P | P | P | P | P | D | P | |||||||||
460.13 | P | P (in qtz) | P | P | P | P | P | P | P | ||||||||
473.61 | P | P | P | P | P | P | P | ||||||||||
475.34 | P | P (in qtz) | P | P | P | P | P | epidote? | P | P | P | ||||||
480.68 | ? | P | P | P | P | D | P | P | |||||||||
481.22 | P | P (in qtz) | P | P | P | P | |||||||||||
486.03 | P | P (in qtz) | P | P | P | D | D | P | |||||||||
495.15 | P (in qtz) | P (in qtz) | P (in qtz) | P | P | P | P | P | |||||||||
500.21 | P (in qtz) | P | P | P | P | P | P | ||||||||||
509.36 | P | P | P | P | |||||||||||||
513.17 | P | P | P | P | P | D | |||||||||||
533.26 | P | P (in qtz) | P (in qtz) | P | P (in qtz) | P | P | D | P | ||||||||
543.87 | P | P | P | P | P | P | P | P | |||||||||
550.03 | P | P (in qtz) | P | P | D | P | |||||||||||
571.80 | P | P | P | P | D | P | P | ||||||||||
615.37 | P | P | P | epidote | P | P | |||||||||||
626.18 | P | P (in qtz) | P | P | P | P | P | P | P | P | |||||||
630.38 | P | P (in qtz) | P | P? | D | P | P | P | |||||||||
643.11 | P | P (in qtz) | P | ? | P | P | P | P | P | ||||||||
655.86 | P? | P | P | P | P | D | P | P | P? | ||||||||
681.02 | P (in qtz) | P (in fsp) | P | P | P? | P | D | P | P | P | |||||||
730.87 | P | P | P | P? | epidote? | D | P | P | P | ||||||||
737.35 | P | P | P | P | P | P | D? | D | P | P | |||||||
750.02 | P | P | P | P | P | P | P? | P | P |