Honnorez, Jose J; Alt, Jeffrey C; Honnorez-Guerstein, B-M; Laverne, Christine; Muehlenbachs, Karlis; Ruiz, J; Saltzman, Eric S (1985): (Table 5) Fluid inclusion geothermometry at DSDP Hole 83-504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.804984, In supplement to: Honnorez, JJ et al. (1985): Stockwork-like sulfide mineralization in young oceanic crust: Deep Sea Drilling Project Hole 504B. In: Anderson, RN; Honnorez, J; Becker, K; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 83, 263-282, https://doi.org/10.2973/dsdp.proc.83.110.1985
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 1.227200 * Longitude: -83.730200
Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00
Minimum Elevation: -3460.0 m * Maximum Elevation: -3460.0 m
Event(s):
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
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Honnorez, Jose J | |||
| 2 | Description | Description | Honnorez, Jose J | |||
| 3 | Type | Type | Honnorez, Jose J | Inclusion | ||
| 4 | Homogenization temperature | Th | °C | Honnorez, Jose J | ||
| 5 | Temperature, calculated | T cal | °C | Honnorez, Jose J | Filling. Pressure corrections applied to the homogenization temperatures are assuming a salinity of 3 wt.% equivalent NaCl, 350 bars of pressure and using Potter's (1977) data. | |
| 6 | Comment | Comment | Honnorez, Jose J |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
81 data points
Data
| 1 Sample label | 2 Description | 3 Type | 4 Th [°C] | 5 T cal [°C] | 6 Comment |
|---|---|---|---|---|---|
| 83-504B-80-1,30-32 | Calcite | Primary | 177 | 215 | |
| 83-504B-80-1,30-32 | Calcite | Primary | 165 | 203 | |
| 83-504B-80-1,30-32 | Quartz | Primary | 244 | 282 | |
| 83-504B-80-1,30-32 | Quartz | Secondary | 100 | 138 | Cloudy, altered quartz |
| 83-504B-80-2,91-97 | Quartz | Primary | 190 | 228 | |
| 83-504B-80-2,91-97 | Quartz | Primary | 190 | 228 | |
| 83-504B-80-2,91-97 | Quartz | Secondary | 212 | 250 | Fracture controlled |
| 83-504B-80-2,91-97 | Analcite | Primary | 215 | 253 | Reaction front in which laumontite is replacing analcite |
| 83-504B-80-2,91-97 | Analcite | Primary | 215 | 253 | Reaction front in which laumontite is replacing analcite |
| 83-504B-80-2,91-97 | Analcite | Primary | 212 | 250 | Reaction front in which laumontite is replacing analcite |
| 83-504B-80-2,91-97 | Analcite | Primary | 215 | 253 | Reaction front in which laumontite is replacing analcite |
| 83-504B-81-1,26-30 | Quartz | Primary | 224 | 262 | |
| 83-504B-81-1,26-30 | Quartz | Primary | 300 | 238 | |
| 83-504B-81-1,26-30 | Quartz | Primary | 295 | 333 | |
| 83-504B-81-1,26-30 | Quartz | Primary | 299 | 337 |