Kastner, Miriam (1982): (Appendix C) Minerals at DSDP Hole 64-478 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.819088, In supplement to: Kastner, M (1982): Evidence for two distinct hydrothermal systems in the Guaymas Basin. In: Curray, JR; Moore, DG; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 64, 1143-1157, https://doi.org/10.2973/dsdp.proc.64.154.1982
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 27.096800 * Longitude: -111.507500
Date/Time Start: 1978-12-24T00:00:00 * Date/Time End: 1978-12-24T00:00:00
Minimum DEPTH, sediment/rock: 0.50 m * Maximum DEPTH, sediment/rock: 338.92 m
Event(s):
64-478 * Latitude: 27.096800 * Longitude: -111.507500 * Date/Time: 1978-12-24T00:00:00 * Elevation: -1889.0 m * Penetration: 464 m * Recovery: 297.6 m * Location: North Pacific/Gulf of California/CHANNEL * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 49 cores; 427 m cored; 24 m drilled; 69.7 % recovery
Comment:
Sediment depth is given in mbsf. Between depths 203.5 and 241.3 as well as between 253.3 and 256.9 is sill. After depth 338.92 is thick sill. tr. = traces, X = common, XX = abundant, - = not determined.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Kastner, Miriam | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Plagioclase | Pl | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 4 | Kalifeldspar | Kfs | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 5 | Quartz | Qz | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 6 | Opal-CT | Opal-CT | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 7 | Opal-A | Opal-A | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 8 | - | - | Kastner, Miriam | X-ray diffraction (XRD) | Quartz to feldspar ratio | |
| 9 | Smectite | Sme | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 10 | Illite | Ill | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 11 | - | - | Kastner, Miriam | X-ray diffraction (XRD) | Chlorite to kaolinite ratio | |
| 12 | Clinoptilolite | Cpt | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 13 | Analcime | Anl | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 14 | Calcite | Cal | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 15 | Dolomite | Dol | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 16 | Pyrite | Py | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 17 | Gypsum | Gp | Kastner, Miriam | X-ray diffraction (XRD) | Or anhydrite | |
| 18 | Comment | Comment | Kastner, Miriam |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1601 data points
Data
| 1 Sample label (DSDP/ODP/IODP sample designation) | 2 Depth sed [m] | 3 Pl (X-ray diffraction (XRD)) | 4 Kfs (X-ray diffraction (XRD)) | 5 Qz (X-ray diffraction (XRD)) | 6 Opal-CT (X-ray diffraction (XRD)) | 7 Opal-A (X-ray diffraction (XRD)) | 8 - (Quartz to feldspar ratio, X-r...) | 9 Sme (X-ray diffraction (XRD)) | 10 Ill (X-ray diffraction (XRD)) | 11 - (Chlorite to kaolinite ratio, ...) | 12 Cpt (X-ray diffraction (XRD)) | 13 Anl (X-ray diffraction (XRD)) | 14 Cal (X-ray diffraction (XRD)) | 15 Dol (X-ray diffraction (XRD)) | 16 Py (X-ray diffraction (XRD)) | 17 Gp (Or anhydrite, X-ray diffracti...) | 18 Comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 64-478-1-1,50-54 | 0.50 | X | - | X | - | XX | Q>F | X | X | X | - | - | X | - | X | - | Detrital clay minerals, S = 75% expandable layers in S/I |
| 64-478-1-1,109-111 | 1.10 | X | - | X | - | XX | Q>F | X | X | X | - | - | X | - | X | - | Detrital clay minerals, S = 75% expandable layers in S/I |
| 64-478-1-2,66-68 | 2.20 | X | X | X | - | XX | Q=F | X | X | X | - | - | X | - | X | - | Detrital clay minerals, S = 75% expandable layers in S/I |
| 64-478-1-2,90-97 | 2.40 | X | - | X | - | X | Q>F | X | tr. | - | tr. | - | XX | - | X | - | Detrital clay minerals, S = 75% expandable layers in S/I |
| 64-478-2-1,136-138 | 4.90 | X | - | X | - | X | Q<F | X | tr. | tr. | tr. | - | XX | - | X | - | Detrital clay minerals, S = 75% expandable layers in S/I |
| 64-478-2-3,100-102 | 7.50 | X | X | X | - | XX | Q<=F | X | X | X | X | - | tr. | - | - | - | Detrital clay minerals, S = 75% expandable layers in S/I |
| 64-478-2-4,120-122 | 9.20 | X | - | X | - | XX | Q<=F | X | X | X | X | - | tr. | - | - | - | Detrital clay minerals, S = 75% expandable layers in S/I |
| 64-478-2-5,69-71 | 10.20 | X | - | X | - | XX | Q=F | X | X | - | X | - | X | - | - | - | Relatively much clinoptilolite |
| 64-478-2-6,82-84 | 11.30 | X | - | X | - | XX | Q>=F | X | tr. | - | - | - | X | - | - | - | S = 75% expandable layers S/I |
| 64-478-3-1,49-51 | 13.50 | X | X | X | - | XX | Q=F | X | tr. | - | - | - | X | - | - | - | S = 75% expandable layers S/I |
| 64-478-3-3,72-74 | 16.70 | X | - | X | - | X | Q>F | X | tr. | - | X | - | X | - | X | - | S = 75% expandable layers S/I |
| 64-478-4-1,59-61 | 23.10 | tr. | - | XX | - | X | Q>>F | X | X | - | X | - | tr. | - | X | X | S = 75% expandable layers S/I |
| 64-478-4-3,98-100 | 26.50 | X | - | X | - | X | Q=F | X | X | - | X | - | X | - | - | - | S = 75% expandable layers S/I |
| 64-478-4-5,82-84 | 29.30 | X | X | X | - | X | Q>F | X | X | X | X | - | - | - | - | - | S = 75% expandable layers S/I |
| 64-478-4-6,93-95 | 30.90 | X | X | X | - | XX | Q>F | X | tr. | tr. | X | - | X | - | - | X | S = 75% expandable layers S/I |
| 64-478-5-1,130-135 | 33.30 | X | X | X | - | XX | Q>F | X | tr. | tr. | X | - | X | - | - | X | S = 75% expandable layers S/I |
| 64-478-5-2,75-77 | 34.30 | X | - | X | - | X | Q>F | X | X | X | X | - | X | - | X | - | S = 75% expandable layers S/I |
| 64-478-5-6,40-42 | 39.90 | X | - | X | - | X | Q>F | X | X | X | X | - | X | - | X | - | Some amphibole |
| 64-478-6-1,43-45 | 41.90 | X | - | X | - | X | Q>F | X | X | X | X | - | X | - | X | - | Some amphibole |
| 64-478-6-2,69-71 | 43.70 | X | - | X | - | X | Q>F | X | tr. | tr. | X | - | - | - | X | X | Relatively much clinoptilolite |
| 64-478-6-4,81-83 | 46.80 | X | X | X | - | X | Q>F | X | tr. | tr. | tr. | - | X | - | X | - | |
| 64-478-6-5,27-29 | 47.80 | X | - | X | - | XX | Q>>F | tr. | tr. | tr. | tr. | - | - | - | - | - | |
| 64-478-6-5,51-52 | 48.00 | X | - | X | - | X | Q<F | tr. | X | - | - | - | - | - | X | - | |
| 64-478-7-4,79-81 | 56.30 | X | - | X | - | X | Q>F | tr. | tr. | tr. | - | - | XX | - | X | - | |
| 64-478-7-6,82-84 | 59.30 | X | - | X | - | X | Q=F | X | tr. | - | X | - | X | - | - | - | |
| 64-478-7-7,28-30 | 60.30 | X | - | X | - | XX | Q>F | X | X | - | - | - | X | - | - | - | |
| 64-478-8-1,104-106 | 61.60 | X | - | X | - | X | Q>F | X | X | - | X | - | X | - | X | - | |
| 64-478-8-3,112-114 | 64.60 | X | - | X | - | X | Q>F | X | X | X | X | - | - | - | X | - | |
| 64-478-9-4,15-17 | 74.70 | X | - | X | - | X | Q>F | X | X | X | X | - | X | - | X | - | |
| 64-478-10-2,43-45 | 81.40 | X | - | X | - | X | Q>F | X | X | - | X | - | X | - | X | - | |
| 64-478-11-2,106-108 | 91.60 | X | - | X | - | X | Q>F | X | X | - | X | - | X | - | X | - | |
| 64-478-11-6,50-52 | 96.60 | X | - | X | - | XX | Q>F | X | X | X | X | - | - | - | - | - | |
| 64-478-12-4,104-106 | 104.10 | X | X | X | - | XX | Q>F | X | X | X | X | - | X | - | - | - | |
| 64-478-13-4,102-104 | 113.50 | X | X | X | - | XX | Q>F | X | X | X | X | - | X | - | - | - | |
| 64-478-14-5,138-140 | 124.90 | X | - | X | - | X | Q>>F | X | tr. | - | - | - | X | X | - | X | Some protodolomite |
| 64-478-15-4,133-135 | 132.80 | X | - | X | - | X | Q>F | tr. | tr. | - | X | - | X | X? | X | - | |
| 64-478-16-3,63-65 | 140.10 | X | - | X | - | X | Q>F | X | X | X | X | - | X | - | X | - | |
| 64-478-17-4,97-99 | 151.50 | X | - | X | - | X | Q>F | X | X | X | X | - | tr. | - | X | - | |
| 64-478-18-1,14-18 | 155.70 | X | X | X | - | tr. | Q=F | tr. | tr. | - | - | - | - | - | - | - | Mainly quartz and two feldspars |
| 64-478-19-7,24-26 | 168.80 | X | - | X | - | X | Q>F | X | tr. | - | X | - | tr. | - | X | - | |
| 64-478-21-4,30-32 | 179.30 | X | - | X | - | XX | Q>F | X | X | tr. | X | - | X | - | X | X | |
| 64-478-21-6,55-57 | 182.60 | X | - | X | - | XX | Q>F | X | - | - | tr. | - | X | - | - | X | |
| 64-478-22-1,93-95 | 184.90 | X | - | X | - | X | Q>F | X | tr. | tr. | X | - | X | - | X | X | |
| 64-478-22-2,103-105 | 186.50 | X | - | X | - | X | Q>F | X | tr. | tr. | X | - | X | - | X | tr. | |
| 64-478-22-3,116-118 | 188.20 | X | - | X | - | X | Q>F | X | tr. | tr. | X | - | X | - | X | X | |
| 64-478-22-CC,0-3 | 188.50 | - | - | X | - | - | - | - | - | - | - | - | - | XX | - | - | Mainly dolomite |
| 64-478-22-CC,3-8 | 189.00 | X | - | X | - | - | Q=F | tr. | tr. | - | X | - | - | X | - | - | Dolomite with distinct order reflections |
| 64-478-24-1,0-4 | 203.50 | X | - | X | - | - | Q=F | tr. | tr. | - | XX | - | - | X | X | - | Dolomite with distinct order reflections. Much clinoptilolite |
| 64-478-28-0.29-31 | 241.30 | X | - | X | - | X | Q=F | X | tr. | tr. | X | - | X | - | X | X | S = 100% expandable layers |
| 64-478-21-0.33-35 | 241.30 | X | - | X | - | X | Q=F | X | tr. | tr. | X | - | X | - | X | X | S = 100% expandable layers |
| 64-478-28-1.31-34 | 242.80 | X | - | X | - | X | Q=F | X | tr. | tr. | X | - | X | - | X | X | S = 100% expandable layers |
| 64-478-28-1,117-119 | 243.70 | X | - | X | - | X | Q=F | X | tr. | tr. | X | - | X | - | X | - | |
| 64-478-28-2,8-10 | 244.10 | X | - | X | - | X | Q=F | X | tr. | tr. | - | - | X | - | X | X | |
| 64-478-28-2,23-25 | 244.20 | X | - | X | - | X | Q=F | X | tr. | - | tr. | - | X | - | X | tr. | |
| 64-478-28-2,122-124 | 245.20 | X | - | X | - | X | Q=F | X | tr. | - | X | - | X | - | X | X | |
| 64-478-28-3,35-37 | 245.90 | X | - | X | - | X | Q=F | tr. | tr. | - | tr. | - | X | X | X | X | |
| 64-478-28-3,139-141 | 246.90 | X | - | X | - | XX | Q<=F | X | X | - | - | - | x | - | X | - | Well-crystallized illite |
| 64-478-28-4,23-25 | 247.20 | X | X | X | - | X | Q>F | X | tr. | - | - | - | X | - | X | X | |
| 64-478-28-5,31-33 | 248.80 | X | X | X | - | X | Q>F | X | tr. | - | - | - | - | - | X | tr. | S = 80% expandable layers in S/l |
| 64-478-28-6,6-8 | 249.60 | X | X | X | - | X | Q>F | X | tr. | - | X | - | X | - | X | tr. | |
| 64-478-28-6,52-54 | 250.00 | X | - | X | - | X | Q>=F | X | X | - | X | - | X | - | - | X | |
| 64-478-28-6,105-107 | 250.60 | X | - | X | - | XX | Q<F | X | X | X | X | - | X | - | X | - | |
| 64-478-29-1,26-28 | 250.80 | X | X | X | - | X | Q>F | X | tr. | - | X | - | X | - | X | - | |
| 64-478-29-2,25-26 | 252.30 | X | X | X | - | X | Q>F | X | tr. | - | X | - | X | - | X | X | Much gypsum and much pyrite |
| 64-478-29-2,48-50 | 252.50 | X | - | X | XX | tr. | Q>F | X | tr. | - | - | - | X | - | X | tr. | Much opal-CT; abundant pyrite |
| 64-478-29-2,104-107 | 253.10 | X | - | X | XX | - | Q=F | X | tr. | - | - | X | X | - | X | X | Much opal-CT; S = 100% expandable layers; analcime |
| 64-478-29-2,132-134 | 253.30 | X | - | XX | X | - | Q>=F | X | - | - | - | - | - | - | X | - | Less opal-CT; S = 100% expandable layers and well crystallized |
| 64-478-30-1,35-37 | 256.90 | X | - | X | XX | tr. | Q=F | tr. | tr. | - | XX | - | - | - | X | - | Much clinoptilolite; much opal-CT; relatively much pyrite |
| 64-478-30-1,73-78 | 257.30 | X | - | X | XX | tr. | Q>F | tr. | tr. | - | - | - | X | X? | - | tr. | Much opal-CT |
| 64-478-30-2,10-12 | 258.10 | X | - | X | X? | X | Q=F | X | tr. | - | - | - | X | - | X | tr. | |
| 64-478-30-2,94-96 | 259.00 | X | - | X | - | X | Q>F | X | tr. | - | X | - | X | - | X | - | |
| 64-478-30-CC | 259.50 | X | - | X | - | X | Q=F | X | tr. | - | X | - | X | - | X | - | S = 70% expandable layers in S/l |
| 64-478-31-1,46-48 | 260.50 | X | - | X | - | X | Q=F | X | X | - | - | - | X | - | X | X | |
| 64-478-31-1,142-144 | 261.40 | X | - | X | - | X | Q>F | X | X | - | X | - | - | - | - | tr | |
| 64-478-31-3,64-66 | 263.70 | X | - | X | - | X | Q>F | X | X | - | X | - | X | - | - | - | |
| 64-478-31-5,117-119 | 267.20 | X | - | X | - | X | Q>F | X | X | - | X | - | X | - | - | - | |
| 64-478-32-3,46-48 | 273.00 | X | - | X | - | X | Q>F | X | X | - | X | - | X | - | X | - | |
| 64-478-33-3,50-52 | 282.50 | X | - | X | - | X | Q>F | X | X | - | X | - | X | - | X | - | |
| 64-478-34-1,29-31 | 288.80 | X | - | X | - | tr. | Q>F | X | tr. | - | - | - | X | X? | X | X | |
| 64-478-34-3,88-90 | 292.40 | X | - | X | - | tr. | Q>F | X | tr. | - | - | - | X | X? | X | tr. | |
| 64-478-35-1,38-39 | 298.40 | X | - | X | - | tr. | Q>F | X | tr. | - | - | - | X | X | X | X | |
| 64-478-35-4,86-87 | 303.40 | X | - | X | - | tr. | Q>F | tr. | tr. | - | - | - | - | XX | - | X | Protodolomite is main phase |
| 64-478-35-5,35-37 | 304.40 | X | - | X | - | X | Q=F | X | tr. | tr. | - | - | XX | - | X | - | |
| 64-478-36-2,7-9 | 309.10 | tr. | - | X | - | X | Q>>F | X | tr. | tr. | - | - | XX | - | X | - | |
| 64-478-36-2,41-43 | 309.40 | X | - | X | - | tr. | Q>F | X | tr. | - | - | - | X | X | X | X | |
| 64-478-36-2,94-95 | 310.00 | X | - | X | - | tr. | Q>F | tr. | tr. | - | - | - | X | - | X | - | |
| 64-478-39-2,107-108 | 329.10 | tr. | - | X | X | - | Q>>F | tr. | tr. | - | - | - | X | - | X | tr | Opal-CT = quartz |
| 64-478-39-3,44-46 | 330.00 | X | - | X | X | - | Q>F | tr. | tr. | - | tr. | - | X | - | X | tr. | Opal-CT = quartz |
| 64-478-40-1,3-4 | 336.00 | X | - | X | X | - | Q=F | X | tr. | - | - | - | tr. | - | - | X | Opal-CT = quartz |
| 64-478-40-1,19-21 | 336.20 | X | - | XX | X | - | Q>F | X | - | - | - | - | X | - | X | X | Opal-CT < quartz |
| 64-478-40-1,118-120 | 337.20 | X | - | XX | - | - | Q>=F | tr. | tr. | - | - | - | - | - | XX | tr. | Mainly quartz and feldspar; much pyrite; no opal-CT |
| 64-478-40-2,40-42 | 337.90 | X | - | XX | - | - | Q>=F | X | tr. | - | - | - | X | - | XX | X | Mainly quartz and feldspar; much pyrite; no opal-CT |
| 64-478-40-2,90-99 | 338.50 | X | - | XX | - | - | Q>F | X | tr. | - | - | - | X | - | X | X | Mainly quartz and feldspars; clay crystallinity increases |
| 64-478-40-2,128-129 | 338.78 | X | - | XX | - | - | Q>F | X | X | - | - | - | - | - | tr. | X | Mainly quartz and feldspars; clay crystallinity increases |
| 64-478-40-2,132-133 | 338.82 | X | - | XX | - | - | Q>=F | X | X | - | - | - | X | - | tr. | - | S and I are well crystallized. S = 100% expandable layers. |
| 64-478-40-2,137-138 | 338.87 | X | - | X | - | - | Q=F | XX | - | - | - | - | - | - | - | X | Much well-crystallized S = 100% expandable layers. This sample is mixed with basalt pieces |
| 64-478-40-2,141-143 | 338.92 | X | - | X | - | - | Q<=F | XX | - | - | - | - | - | - | - | X | Much well-crystallized S = 100% expandable layers. This sample is mixed with basalt pieces |