Alt, Jeffrey C; Muehlenbachs, Karlis; Honnorez, Jose J (1986): (Table 1) Oxygen and carbon isotopic composition of secondary minerals from DSDP Hole 504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.713289, In supplement to: Alt, JC et al. (1986): An oxygen isotopic profile through the upper kilometer of the oceanic crust, DSDP Hole 504B. Earth and Planetary Science Letters, 80(3-4), 217-229, https://doi.org/10.1016/0012-821X(86)90106-8
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 1.227100 * Median Longitude: -83.730100 * South-bound Latitude: 1.227000 * West-bound Longitude: -83.730200 * North-bound Latitude: 1.227200 * East-bound Longitude: -83.730000
Date/Time Start: 1979-12-04T00:00:00 * Date/Time End: 1982-01-02T00:00:00
Minimum DEPTH, sediment/rock: 252 m * Maximum DEPTH, sediment/rock: 1045 m
Event(s):
70-504B * Latitude: 1.227000 * Longitude: -83.730000 * Date/Time: 1979-12-04T00:00:00 * Elevation: -3460.0 m * Penetration: 836.1 m * Recovery: 91.6 m * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 328.6 m cored; 18.5 m drilled; 27.9 % recovery
83-504B * Latitude: 1.227200 * Longitude: -83.730200 * Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00 * Elevation: -3460.0 m * Penetration: 1350 m * Recovery: 107.7 m * Campaign: Leg83 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: Leg 83 of DSDP was devoted entirely to coring and experiments in Hole 504B, the deepest borehole to date into the oceanic crust. Hole 504B now extends over a kilometer into basement, nearly twice as far as any other DSDP hole, and it is the only DSDP hole to have clearly penetrated into the intrusive sheeted dikes that underlie the extrusive pillow lavas of the upper oceanic crust. At Hole 504B, Leg 83 continued an ongoing DSDP effort that began during Legs 68, 69, and 70 in 1979, and also included part of Leg 92 in 1983. 71 cores; 514 m cored; 0 m drilled; 21 % recovery
Comment:
Depth, sediment (m) is the sub-basement depth (m)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Sample code/label | Sample label | Alt, Jeffrey C | DSDP/ODP/IODP sample designation | ||
| 4 | δ18O | δ18O | ‰ | Alt, Jeffrey C | clay (per mil SMOW) | |
| 5 | δ18O | δ18O | ‰ | Alt, Jeffrey C | quartz (per mil SMOW) | |
| 6 | δ18O | δ18O | ‰ | Alt, Jeffrey C | epidote (per mil SMOW) | |
| 7 | δ18O | δ18O | ‰ | Alt, Jeffrey C | carbonate (per mil SMOW) | |
| 8 | δ18O | δ18O | ‰ | Alt, Jeffrey C | analcite/gyrohte (per mil SMOW) | |
| 9 | δ13C | δ13C | ‰ PDB | Alt, Jeffrey C | carbonate (per mil PDB) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
82 data points
Data
| 1 Event | 2 Depth sed [m] | 3 Sample label | 4 δ18O [‰] (clay (per mil SMOW)) | 5 δ18O [‰] (quartz (per mil SMOW)) | 6 δ18O [‰] (epidote (per mil SMOW)) | 7 δ18O [‰] (carbonate (per mil SMOW)) | 8 δ18O [‰] (analcite/gyrohte (per mil SMOW)) | 9 δ13C [‰ PDB] (carbonate (per mil PDB)) |
|---|---|---|---|---|---|---|---|---|
| 70-504B | 252 | 70-504B-34-1,7-19 | 32.9 | -0.2 | ||||
| 70-504B | 260 | 70-504B-35-1,2-4 | 24.4 | -0.3 | ||||
| 70-504B | 261 | 70-504B-35-1,136-139 | 28.7 | -0.3 | ||||
| 70-504B | 278 | 70-504B-37-1,36-38 | 28.7 | 0.3 | ||||
| 70-504B | 279 | 70-504B-37-1,76-80 | 11.2 | 17.8 | ||||
| 70-504B | 279 | 70-504B-37-1,94-96 | 13.4 | 18.2 | ||||
| 70-504B | 286 | 70-504B-37-3,32-34 | 31.5 | 0.0 | ||||
| 70-504B | 310 | 70-504B-40-3,130-135 | 28.0 | -0.1 | ||||
| 70-504B | 341 | 70-504B-44-2,97-99 | 31.5 | -1.1 | ||||
| 70-504B | 376 | 70-504B-48-3,14-18 | 13.2 | 13.9 | ||||
| 70-504B | 413 | 70-504B-53-1,3-5 | 23.7 | -1.8 | ||||
| 83-504B | 580 | 83-504B-73-2,29-32 | 10.0 | -2.5 | ||||
| 83-504B | 632 | 83-504B-79-2,97-100 | 8.4 | |||||
| 83-504B | 635 | 83-504B-79-3,147-149 | 18.0 | -7.7 | ||||
| 83-504B | 636 | 83-504B-80-1,30-32 | 11.5 | 9.6 | -6.1 | |||
| 83-504B | 637 | 83-504B-80-1,106-111 | 1.3 | 11.1 | 10.6 | -5.1 | ||
| 83-504B | 638 | 83-504B-80-2,63-67 | 13.3 | -5.0 | ||||
| 83-504B | 638 | 83-504B-80-2,91-97 | 9.8 | |||||
| 83-504B | 655 | 83-504B-82-1,68-73 | 18.2 | -10.7 | ||||
| 83-504B | 674 | 83-504B-84-2,36-40 | 18.4 | 2.4 | ||||
| 83-504B | 721 | 83-504B-90-1,69-72 | 7.7 | 2.5 | ||||
| 83-504B | 739 | 83-504B-92-1,128-131 | 12.1 | -5.0 | ||||
| 83-504B | 742 | 83-504B-92-3,112-113 | 8.4 | 2.3 | ||||
| 83-504B | 766 | 83-504B-95-1,54-59 | 2.8 | 15.6 | -4.8 | |||
| 83-504B | 798 | 83-504B-99-1,70-74 | 3.1 | |||||
| 83-504B | 806 | 83-504B-100-1,14-18 | 8.6 | |||||
| 83-504B | 870 | 83-504B-107-1,90-92 | 11.7 | |||||
| 83-504B | 1045 | 83-504B-135-1,4-9 | 9.9 |