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Alt, Jeffrey C; Muehlenbachs, Karlis; Honnorez, Jose J (1986): (Table 3) Oxygen isotopic composition and calculated equilibrium temperatures of formation of quartz-epidote pairs from DSDP Hole 504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.713294, 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):
Coverage:
Latitude: 1.227200 * Longitude: -83.730200
Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00
Minimum DEPTH, sediment/rock: 674 m * Maximum DEPTH, sediment/rock: 742 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
Comment:
Depth, sediment (m) is the sub-basement depth (m)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2Sample code/labelSample labelAlt, Jeffrey CDSDP/ODP/IODP sample designation
3δ18Oδ18OAlt, Jeffrey Cquartz (per mil SMOW)
4δ18Oδ18OAlt, Jeffrey Cepidote (per mil SMOW)
5δ18Oδ18OAlt, Jeffrey Ccalculated fluid d18O (per mil SMOW) after Clayton et al. 1972, doi:10.1029/JB077i017p03057)
6Temperature, calculatedT cal°CAlt, Jeffrey Cformation temperature, assuming 23 % substitution of Fe for Al in epidote (Matthews and Shliestedt 1984, doi:10.1007/BF00371419)
Size:
15 data points

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