Anderson, Thomas F (1980): (Table 1) Stratigraphic Information on the carbonate veins at DSDP Leg 58 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.821398, In supplement to: Anderson, TF (1980): Stable-isotope evidence for the origin of secondary carbonate veins in Deep Sea Drilling Project Leg 58 basalts. In: deVries Klein, G; Kobayashi, K; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 58, 905-911, https://doi.org/10.2973/dsdp.proc.58.137.1980
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 27.912425 * Median Longitude: 135.989075 * South-bound Latitude: 24.700700 * West-bound Longitude: 132.774800 * North-bound Latitude: 29.327500 * East-bound Longitude: 137.683800
Date/Time Start: 1977-12-12T00:00:00 * Date/Time End: 1978-01-18T00:00:00
Minimum DEPTH, sediment/rock: 246 m * Maximum DEPTH, sediment/rock: 571 m
Event(s):
58-442B * Latitude: 28.984000 * Longitude: 136.057200 * Date/Time: 1977-12-12T00:00:00 * Elevation: -4634.0 m * Penetration: 455 m * Recovery: 51 m * Location: North Pacific/BASIN * Campaign: Leg58 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 187.5 m cored; 0 m drilled; 27.2 % recovery
58-443 * Latitude: 29.327500 * Longitude: 137.440500 * Date/Time: 1977-12-28T00:00:00 * Elevation: -4372.0 m * Penetration: 581.5 m * Recovery: 300 m * Location: North Pacific/BASIN * Campaign: Leg58 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 64 cores; 581.5 m cored; 0 m drilled; 51.6 % recovery
58-444A * Latitude: 28.637500 * Longitude: 137.683800 * Date/Time: 1978-01-04T00:00:00 * Elevation: -4843.0 m * Penetration: 310 m * Recovery: 105.7 m * Location: North Pacific/BASIN * Campaign: Leg58 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 218.5 m cored; 0 m drilled; 48.4 % recovery
Comment:
Sediment depth is given in mbsf. Volcanic sequence begins at sub-bottom depths of 290 m in Hole 58-442B and 457 m in Hole 58-443.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Sample code/label | Sample label | Anderson, Thomas F | DSDP/ODP/IODP sample designation | ||
| 6 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 7 | Lithologic unit/sequence | Unit | Anderson, Thomas F | |||
| 8 | Thickness | Thick | m | Anderson, Thomas F | #1 = 1 for unit IV-B / 9 for unit IV-C; ?0 = unknown | |
| 9 | Location | Location | Anderson, Thomas F | In unit |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
68 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Depth sed [m] | 7 Unit | 8 Thick [m] | 9 Location |
|---|---|---|---|---|---|---|---|---|
| 58-442B | 28.9840 | 136.0572 | -4634 | 58-442B-6-2,134-137 | 318 | I-G | 2.0 | 100 cm below the upper chill boundary. |
| 58-442B | 28.9840 | 136.0572 | -4634 | 58-442B-8-7,124-128 | 343 | I-L | 1.5 | 20 cm above the lower chill boundary. |
| 58-442B | 28.9840 | 136.0572 | -4634 | 58-442B-9-3,80-84 | 347 | I-O | 5.0 | Near the center of the unit |
| 58-442B | 28.9840 | 136.0572 | -4634 | 58-442B-10-2,16-19 | 335 | II | ?0.0 | 150 cm below the top of the pillow-lava sequence, which is apparently overlain by a few meters of fossil_iferous mud. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-50-2,36-39 | 465 | I-A | 16.0 | Near the center of the unit. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-53-2,87-89 | 484 | I-C | 3.0 | In the bottom third of the unit. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-55-2,93-95 | 503 | II-A | 4.0 | In the basal zone of pillow-lava unit overlain by an intraformational limestone breccia. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-56-4,24-27 | 509 | II-B | 8.0 | In the lower part of the unit; 6 cm of limestone and chalk are at the base. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-58-3,77-90 | 524 | II-D | 5.0 | In the lower part of the unit. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-59-1,95-98 | 531 | II-F | 2.0 | In the lower part of the unit; 12 cm of nannofossil chalk and limestone are at the base. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-59-5,84-88 | 535 | II-H | 2.0 | Immediately above the basal chill zone. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-61-3,119-124 | 552 | IV-B/IV-C | #1.0 | In the chill margin between the two units. |
| 58-443 | 29.3275 | 137.4405 | -4372 | 58-443-63-3,25-30 | 571 | IV-E | 11.0 | In the upper part of the unit. |
| 58-444A | 28.6375 | 137.6838 | -4843 | 58-444A-20-2,131-133 | 246 | I | 12.0 | In the upper part of the sill; 21 m of mud stone underlies the sill. |
| 58-444A | 28.6375 | 137.6838 | -4843 | 58-444A-27-5,17-19 | 306 | II | ?0.0 | 34 m below the top of the unit, 1 m above the base of the hole. |
| 58-446A | 24.7007 | 132.7748 | -4952 | 58-446A-4-1,66-72 | 401 | II-A | 16.0 | 5 m below the top of the sill. |
| 58-446A | 24.7007 | 132.7748 | -4952 | 58-446A-13-1,80-84 | 477 | V-A | 4.0 | Near the lower chill margin. |