Kastner, Miriam (1982): (Appendix B) Minerals at DSDP Site 64-481 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.819087, 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: 27.253000 * Longitude: -111.507700
Date/Time Start: 1979-01-03T00:00:00 * Date/Time End: 1979-01-03T00:00:00
Minimum DEPTH, sediment/rock: 2.2 m * Maximum DEPTH, sediment/rock: 346.3 m
Event(s):
64-481 * Latitude: 27.253000 * Longitude: -111.507700 * Date/Time: 1979-01-03T00:00:00 * Elevation: -1998.0 m * Penetration: 52.3 m * Recovery: 33.2 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 48 m cored; 4.8 m drilled; 69.2 % recovery
64-481A * Latitude: 27.253000 * Longitude: -111.507700 * Date/Time: 1979-01-03T00:00:00 * Elevation: -1998.0 m * Penetration: 374.5 m * Recovery: 159 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 31 cores; 293.5 m cored; 39 m drilled; 54.2 % recovery
Comment:
Sediment depth is given in mbsf. Between depths 170.6 and 203.6 and after 346.3 is sill. Between 322.7 and 346.3 is thin sill. tr. = traces, X = common, XX = abundant, - = not determined.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Kastner, Miriam | DSDP/ODP/IODP sample designation | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 4 | Plagioclase | Pl | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 5 | Kalifeldspar | Kfs | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 6 | Quartz | Qz | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 7 | Opal-CT | Opal-CT | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 8 | Opal-A | Opal-A | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 9 | - | - | Kastner, Miriam | X-ray diffraction (XRD) | Quartz to feldspar ratio | |
| 10 | Smectite | Sme | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 11 | Illite | Ill | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 12 | - | - | Kastner, Miriam | X-ray diffraction (XRD) | Chlorite to kaolinite ratio | |
| 13 | Clinoptilolite | Cpt | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 14 | Analcime | Anl | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 15 | Calcite | Cal | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 16 | Siderite | Sd | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 17 | Pyrite | Py | Kastner, Miriam | X-ray diffraction (XRD) | ||
| 18 | Gypsum | Gp | Kastner, Miriam | X-ray diffraction (XRD) | Or anhydrite | |
| 19 | Comment | Comment | Kastner, Miriam |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1383 data points
Data
| 1 Event | 2 Sample label (DSDP/ODP/IODP sample designation) | 3 Depth sed [m] | 4 Pl (X-ray diffraction (XRD)) | 5 Kfs (X-ray diffraction (XRD)) | 6 Qz (X-ray diffraction (XRD)) | 7 Opal-CT (X-ray diffraction (XRD)) | 8 Opal-A (X-ray diffraction (XRD)) | 9 - (Quartz to feldspar ratio, X-r...) | 10 Sme (X-ray diffraction (XRD)) | 11 Ill (X-ray diffraction (XRD)) | 12 - (Chlorite to kaolinite ratio, ...) | 13 Cpt (X-ray diffraction (XRD)) | 14 Anl (X-ray diffraction (XRD)) | 15 Cal (X-ray diffraction (XRD)) | 16 Sd (X-ray diffraction (XRD)) | 17 Py (X-ray diffraction (XRD)) | 18 Gp (Or anhydrite, X-ray diffracti...) | 19 Comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 64-481 | 64-481-1-2,66-68 | 2.2 | X | X | X | - | XX | Q<F | X | tr. | tr. | tr. | - | X | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-2-1,10-12 | 4.9 | X | X | X | - | XX | Q<F | X | tr. | tr. | tr. | - | X | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-2-1,145-150 | 6.2 | X | X | X | - | XX | Q<F | X | X | X | tr. | - | X | - | ir. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-2-2,8-9 | 6.3 | X | X | X | - | XX | Q<=F | X | X | tr. | X | - | XX | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-2-3,41-43 | 8.2 | X | - | X | - | XX | Q=F | tr. | tr. | tr. | X | - | X | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-3-1,129-131 | 10.8 | X | X | X | - | X | Q>=F | X | X | tr. | tr. | - | XX | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-3-2,110-112 | 12.1 | X | X | X | - | X | Q<=F | X | X | tr. | tr. | - | XX | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-4-1,23-25 | 14.5 | X | X | X | - | X | Q>F | X | X | X | tr. | - | X | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-4-1,40-42 | 14.7 | X | X | X | - | XX | Q<F | X | X | tr. | X | - | XX | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-6-1,15-16 | 23.4 | X | - | X | - | XX | Q>F | X | X | tr. | X | - | X | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-7-1,72-74 | 29.2 | X | X | X | - | XX | Q=F | X | X | X | tr. | - | X | - | X | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-7-CC,17-19 | 33.2 | X | - | X | - | XX | Q>F | X | X | tr. | - | - | X | - | - | X | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-8-1,87-89 | 34.1 | X | X | X | - | XX | Q>>F | X | X | tr. | tr. | - | X | - | tr. | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-8-2,143-145 | 36.2 | X | - | X | - | X | Q>F | X | X | XX | - | - | - | - | tr. | - | Much chlorite in clay fraction (Mg > Fe), moderate S/I. Possible an altered ash layer |
| 64-481 | 64-481-8-3,3-5 | 36.3 | tr. | - | X | - | - | Q>>F | X | X | XX | - | - | - | - | tr. | - | Much chlorite in clay fraction (Mg > Fe), moderate S/I. Possible an altered ash layer |
| 64-481 | 64-481-8-3,9-11 | 36.4 | X | - | XX | - | - | Q>F | X | - | XX | - | - | - | - | - | - | Much chlorite in clay fraction (Mg > Fe), moderate S/I. Possible an altered ash layer |
| 64-481 | 64-481-8-3,112-113 | 37.4 | X | - | X | - | X | Q=F | X | tr. | tr. | X | - | X | - | X | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-8-CC,5-7 | 37.8 | X | - | X | - | X | Q=F | X | tr. | tr. | X | - | X | - | - | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-9-1,140-150 | 39.5 | X | X | X | - | X | Q<F | X | X | tr. | - | - | X | - | X | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-10-1,41-42 | 43.2 | X | - | X | - | X | Q<F | X | X | - | - | - | X | - | X | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-10-1,97-99 | 43.7 | X | X | X | - | X | Q<F | X | - | X | tr. | - | X | - | - | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-10-3,86-88 | 46.6 | X | - | X | - | X | Q>F | X | X | - | - | - | tr. | - | X | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481 | 64-481-11-1,23-25 | 47.7 | X | - | X | - | X | Q=F | X | X | - | - | - | X | - | X | - | S = 75% to 80% expandable layers in mixed layer S/I |
| 64-481A | 64-481A-1-2,56-58 | 44.1 | X | X | X | - | X | Q=F | X | X | X | tr. | - | - | - | X | - | S = 75% expandable layers in mixed layer S/I |
| 64-481A | 64-481A-2-1,87-88 | 52.4 | X | X | X | - | X | Q=F | X | X | tr. | X | - | - | - | - | - | S = 75% expandable layers in mixed layer S/I |
| 64-481A | 64-481A-3-1,101-103 | 62.0 | X | X | X | - | X | Q=F | X | X | tr. | tr. | - | - | - | - | X | S = 75% expandable layers in mixed layer S/I |
| 64-481A | 64-481A-4-1,19-21 | 70.7 | X | - | X | - | X | Q>F | X | - | X | tr. | - | X | - | X | - | S = 75% expandable layers in mixed layer S/I |
| 64-481A | 64-481A-4-3,17-19 | 73.7 | X | - | X | - | X | Q>F | X | - | X | tr. | - | X | - | X | - | S = 75% expandable layers in mixed layer S/I |
| 64-481A | 64-481A-5-2,57-58 | 82.1 | X | X | X | - | XX | Q<<F | X | tr | tr. | tr. | - | X | - | - | - | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-5-7,35-37 | 89.4 | X | X | X | - | XX | Q>F | X | tr. | tr. | X | - | X | - | - | - | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-6-3,28-30 | 92.8 | X | - | X | - | XX | Q>F | X | tr. | tr. | X | - | tr. | - | - | - | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-6-5,58-60 | 96.1 | X | X | X | - | XX | Q<F | X | tr. | tr. | X | - | tr. | - | - | - | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-6-7,7-9 | 98.6 | X | - | X | - | XX | Q>F | u. | tr. | tr. | X | - | - | - | - | - | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-7-3,85-87 | 102.9 | X | - | X | - | XX | Q>=F | X | tr | tr. | X | - | tr. | - | tr. | - | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-7-6,98-100 | 107.5 | X | - | X | - | XX | Q>=F | X | tr. | tr. | X | - | tr. | - | tr. | - | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-8-3,85-87 | 112.4 | X | X | X | - | XX | Q>=F | X | tr. | tr. | X | - | - | - | tr. | X | S = 75% expandable layers in S/I. Significant amounts of clinoptilolite |
| 64-481A | 64-481A-8-6,25-27 | 116.3 | X | - | X | - | X | Q>F | X | tr. | - | X | - | tr. | - | - | - | Less cllnoptilolite than in above samples |
| 64-481A | 64-481A-9-6,56-58 | 126.1 | X | X | X | - | X | Q>F | X | tr. | - | X | - | X | - | - | - | Less cllnoptilolite than in above samples |
| 64-481A | 64-481A-10-4,82-84 | 132.8 | X | X | X | - | X | Q=F | X | tr. | - | X | - | X | - | X | - | Less cllnoptilolite than in above samples. Small amounts of opal-A |
| 64-481A | 64-481A-10-5,24-26 | 133.8 | X | - | X | - | tr. | Q>=F | X | X | - | X | - | - | - | - | - | Less cllnoptilolite than in above samples. Small amounts of opal-A |
| 64-481A | 64-481A-11-2,144-146 | 139.9 | X | - | XX | - | tr. | Q>F | X | tr. | - | - | - | X | - | X | - | No clinoptilolite |
| 64-481A | 64-481A-11-3,9-11 | 140.1 | X | - | XX | - | - | Q>F | X | tr. | - | tr. | - | X | - | - | X | No opal-A |
| 64-481A | 64-481A-12-4,38-40 | 151.4 | X | - | XX | - | - | Q>=F | X | tr. | - | - | - | X | - | - | X | |
| 64-481A | 64-481A-12-5,39-41 | 152.9 | XX | - | XX | - | - | Q<F | X | - | - | - | - | - | - | X | - | Feldspar and quartz dominate; better crystallized S |
| 64-481A | 64-481A-13-1,114-116 | 157.2 | XX | - | XX | - | - | Q<F | X | tr. | - | - | - | X | - | X | X | Feldspar and quartz dominate; better crystallized S |
| 64-481A | 64-481A-13-4,67-69 | 161.2 | XX | X | XX | - | - | Q<F | X | tr. | - | - | - | X | - | X | - | Feldspar and quartz dominate; better crystallized S |
| 64-481A | 64-481A-13-CC,20 | 163.7 | XX | X | XX | - | - | Q<F | X | X | - | - | - | X | - | X | - | Well-crystallized clay minerals |
| 64-481A | 64-481A-14-1,49-51 | 166.0 | XX | - | XX | - | - | Q=F | X | X | - | - | - | X | - | - | - | Mainly quartz and feldspar; well-crystallized I |
| 64-481A | 64-481A-14-1,131-141 | 166.9 | XX | - | XX | - | - | Q=F | X | X | - | - | - | X | - | - | - | Mainly quartz and feldspar; well-crystallized I |
| 64-481A | 64-481A-14-2,99-101 | 168.0 | XX | - | XX | - | - | Q=F | X | tr. | - | - | - | - | - | - | - | Mainly quartz and feldspar; well-crystallized S |
| 64-481A | 64-481A-14-2,141-143 | 168.4 | XX | - | XX | X? | - | Q=F | tr. | tr. | - | - | - | - | - | - | X | Mainly, quartz and feldspar; small amounts of S and I well crystallized |
| 64-481A | 64-481A-14-3,47-49 | 169.0 | XX | - | XX | - | - | Q=F | tr. | tr. | tr. | - | - | tr. | - | X | X | Mainly quartz and feldspar; small amounts of S and I well crystallized |
| 64-481A | 64-481A-14-3,125-127 | 169.8 | XX | - | XX | - | - | Q=F | - | X | X | - | - | X | - | X | X | Mainly quartz and feldspar; well-crystallized I and chlorite (Mg = Fe) |
| 64-481A | 64-481A-14-3,140-150 | 169.9 | XX | - | XX | - | - | Q>=F | tr. | X | X | - | X | X | X | - | - | Mainly quartz and feldspar; well-crystallized I and chlorite (Mg = Fe) |
| 64-481A | 64-481A-14-4,29-31 | 170.3 | XX | X | XX | - | - | Q<=F | tr. | X | X | - | - | X | - | - | - | Mainly, quartz and feldspar; well-crystallized I and chlorite (Mg = Fe). Possibly some native sulfur |
| 64-481A | 64-481A-14-4,44-47 | 170.4 | XX | - | XX | - | - | Q=F | tr. | X | X | - | - | X | - | X | X | Mainly quartz and feldspar; some well-crystallized S, I, Ch |
| 64-481A | 64-481A-14-4,54-55 | 170.6 | XX | X | XX | - | - | Q>F | tr. | X | tr. | - | - | - | - | - | X | Mainly quartz and feldspar; small amounts of well-crystallized clay minerals - mainly I |
| 64-481A | 64-481A-18-1,14-18 | 203.6 | XX | - | XX | - | - | Q>F | tr. | tr. | tr. | - | - | - | - | X | - | Very small amounts of clay minerals |
| 64-481A | 64-481A-18-1,32-35 | 203.8 | XX | X | XX | - | - | Q=F | X | tr. | tr. | - | - | - | - | X | - | Very small amounts of clay minerals; S is the main day |
| 64-481A | 64-481A-18-1,114-116 | 204.7 | XX | - | XX | - | - | Q>F | X | tr. | tr. | - | - | - | - | X | - | |
| 64-481A | 64-481A-20-1,99-101 | 223.5 | X | - | X | - | X | Q>F | X | tr. | tr. | X | - | X | - | X | - | S = 75% expandable layers in mixed-layer S/I |
| 64-481A | 64-481A-20-2,14-16 | 224.2 | X | - | X | - | X | Q=F | X | - | - | X | - | - | - | X | - | S = 75% expandable layers in mixed-layer S/I |
| 64-481A | 64-481A-22-1,140-142 | 242.9 | X | - | X | - | X | Q>F | X | tr. | - | X | - | XX | - | X | - | S = 75% expandable layers in mixed-layer S/I |
| 64-481A | 64-481A-22-2,6-8 | 243.1 | X | X | X | - | XX | Q<=F | X | X | X | X | - | X | X? | - | - | S = 75% expandable layers in mixed-layer S/I |
| 64-481A | 64-481A-22-5,92-94 | 248.4 | X | - | X | - | X | Q<=F | X | - | - | - | - | X | - | X | - | S = 75% expandable layers in mixed-layer S/I |
| 64-481A | 64-481A-24-1,144-146 | 262.0 | X | X | X | - | XX | Q<=F | X | X | - | X | - | X | X | - | - | S = 75% expandable layers in mixed-layer S/I |
| 64-481A | 64-481A-24-3,144-147 | 265.0 | X | - | X | - | X | Q>F | X | X | - | X | - | XX | - | - | X | S = 75% expandable layers in mixed-layer S/I |
| 64-481A | 64-481A-24-5,76-78 | 267.3 | X | - | X | - | XX | Q=F | X | X | tr. | X | - | X | - | tr. | - | Significant amounts of clinopUlolite |
| 64-481A | 64-481A-24-7,94-96 | 270.5 | X | - | X | - | X | Q>F | X | tr. | tr. | tr. | - | X | X? | - | - | |
| 64-481A | 64-481A-25-1,124-126 | 271.3 | X | X | X | X | X | Q<F | X | X | X | X | - | X | - | - | - | |
| 64-481A | 64-481A-25-5,66-68 | 276.7 | X | - | X | - | X | Q>F | X | tr. | tr. | - | - | X | - | tr. | - | |
| 64-481A | 64-481A-26-2,19-21 | 281.2 | X | - | X | - | X | Q>F | X | tr. | - | - | - | X | - | - | - | Laminated sample |
| 64-481A | 64-481A-26-6,90-92 | 287.9 | X | X | X | - | X | Q>F | X | tr. | - | tr. | - | X | X | - | - | Laminated sample |
| 64-481A | 64-481A-26-6,140-150 | 288.5 | X | - | X | - | X | Q=F | X | tr. | - | X | - | X | - | - | - | |
| 64-481A | 64-481A-27-2,52-54 | 291.0 | X | - | X | - | X | Q>F | X | tr. | - | - | - | X | - | X | - | |
| 64-481A | 64-481A-27-3,53-54 | 292.5 | X | - | X | - | X | Q=F | X | X | - | tr. | X? | X | - | - | - | |
| 64-481A | 64-481A-27-7,30-32 | 298.3 | X | - | X | - | X | Q>F | X | tr. | - | X | - | X | - | X | - | |
| 64-481A | 64-481A-28-4,58-60 | 303.6 | X | - | X | - | X | Q>F | X | tr. | - | X | - | X | - | X | - | |
| 64-481A | 64-481A-28-5,140-150 | 306.0 | X | - | X | - | X | Q>=F | X | - | - | X | - | X | - | - | X | |
| 64-481A | 64-481A-30-1,47-48 | 318.0 | X | - | X | - | X | Q>F | tr. | tr. | - | - | - | X | - | - | - | Very small amounts of clay minerals |
| 64-481A | 64-481A-30-4,64-66 | 322.7 | X | - | X | - | X | Q>F | tr. | tr. | - | X | - | XX | - | tr. | - | Laminated sample; not much clay minerals |
| 64-481A | 64-481A-33-1,29-31 | 346.3 | X | - | XX | X | - | Q>F | X | tr. | - | - | X | - | - | - | - | Sample between two sills. S = 100% expandable layers and very well crystallized |