Kastner, Miriam (1982): (Appendix A) Minerals at DSDP Site 64-477 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.819086, 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:
Median Latitude: 27.030400 * Median Longitude: -111.399550 * South-bound Latitude: 27.030000 * West-bound Longitude: -111.400300 * North-bound Latitude: 27.030800 * East-bound Longitude: -111.398800
Date/Time Start: 1978-12-18T00:00:00 * Date/Time End: 1978-12-18T00:00:00
Minimum DEPTH, sediment/rock: 3.3 m * Maximum DEPTH, sediment/rock: 247.5 m
Event(s):
64-477 * Latitude: 27.030800 * Longitude: -111.400300 * Date/Time: 1978-12-18T00:00:00 * Elevation: -2003.0 m * Penetration: 191 m * Recovery: 50.6 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 21 cores; 172 m cored; 19 m drilled; 29.4 % recovery
64-477A * Latitude: 27.030000 * Longitude: -111.398800 * Date/Time: 1978-12-18T00:00:00 * Elevation: -2003.0 m * Penetration: 267 m * Recovery: 16 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 111 m cored; 9.5 m drilled; 14.4 % recovery
Comment:
Sediment depth is given in mbsf. Between depths 50.4 and 105.6 m is sill. Blanks indicate that the mineral was not observed. 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-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 | Minerals | Minerals | Kastner, Miriam | X-ray diffraction (XRD) | Other | |
| 19 | Comment | Comment | Kastner, Miriam |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
560 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-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 Minerals (Other, X-ray diffraction (XRD)) | 19 Comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 64-477 | 64-477-2-2,84-86 | 3.3 | X | X | X | XX | Q<F | X | X | X | tr. | - | X | - | tr. | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-2-3,140-150 | 5.4 | X | X | X | XX | Q=F | X | X | X | tr. | - | - | - | tr. | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-3-1,140-150 | 11.9 | X | X | X | XX | Q=F | X | X | X | X | - | X | - | tr. | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-3-2,72-74 | 12.7 | X | tr. | X | XX | Q<F | X | X | X | - | - | X | - | tr. | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-3-4,21-22 | 15.2 | X | - | X | XX | Q<F | X | X | X | tr. | - | X | - | - | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-4-1,51-53 | 20.5 | X | - | X | XX | Q<F | X | X | - | X | - | X | - | - | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-4-1,133-140 | 21.3 | X | X | X | XX | Q=F | tr. | tr. | - | X | - | - | - | X | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-5-1,140-150 | 30.9 | X | - | X | XX | Q=F | X | tr. | - | X | - | X | - | - | - | S = 75% expandable layers in mixed-layer S/I | |
| 64-477 | 64-477-5-2,53-55 | 31.5 | X | - | X | XX | Q<F | X | X | X | X | - | X | - | X | - | ||
| 64-477 | 64-477-7-1,36-38 | 48.9 | X | - | XX | X | Q>F | X | tr. | - | tr. | - | - | - | X | X | S = no Illite layers | |
| 64-477 | 64-477-7-1,140-150 | 49.9 | X | - | XX | tr. | Q=F | X | - | - | - | X | X | tr. | X | X | An amphibole | S = no vertical layers, well crystallized |
| 64-477 | 64-477-7-2,35-37 | 50.4 | XX | - | XX | - | Q<=F | XX | tr. | - | - | - | - | - | X | X | Possibly goethite | S = no vertical layers, well crystallized |
| 64-477 | 64-477-15-1,7-9 | 105.6 | tr. | X | X | - | Q>F | X | - | tr. | - | - | - | X | X | - | S = no vertical layers, well crystallized; D = protodolomite; AF = hydrothermal | |
| 64-477 | 64-477-15-1,126-131 | 106.3 | X | X | XX | - | Q>F | X | tr. | tr. | - | - | - | - | X | X | S = 75% expandable layers in S/I | |
| 64-477 | 64-477-16-1,10-11 | 115.1 | X | tr. | X | X | Q>F | tr. | tr. | - | - | - | - | XX | X | X | D = protodolomite; gypsum and anhydrite | |
| 64-477 | 64-477-16-4,140-150 | 120.9 | X | X | X | - | Q>F | - | X | X | - | - | - | - | X | X | First appearance of greenschist-facies chlorite; Q > Ch>> Pl; Pl = albite | |
| 64-477 | 64-477-17-2,51-53 | 126.5 | X | tr. | X | - | Q=F | - | X | X | - | - | - | - | X | X | Plagioclase albite | |
| 64-477 | 64-477-17-2,140-150 | 127.4 | X | tr. | X | - | Q>F | tr. | tr. | X | - | - | - | - | X | X | Some epidote (possiblynatrolite) | Plagioclase albite |
| 64-477 | 64-477-19-1,140-150 | 144.9 | X | tr. | X | - | O<=F | tr. | tr. | X | - | - | X | - | - | X | Some epidote and sphene | Plagioclase albite |
| 64-477 | 64-477-20-1,140-150 | 154.4 | X | tr. | X | - | Q=F | - | tr. | X | - | - | X | - | X | X | Sphene and some epidote | Plagioclase albite |
| 64-477 | 64-477-22-1,140-150 | 173.4 | XX | - | XX | - | Q=F | - | - | X | - | - | X | - | X | X | Sphene | Plagioclase albite |
| 64-477 | 64-477-23-0-CC | 181.5 | X | - | X | - | Q=F | - | - | XX | - | - | X | - | X | - | Much pyrrhotite | Plagioclase albite |
| 64-477 | 64-477-23-1,34-36 | 181.8 | X | - | X | - | Q=F | - | - | XX | - | - | X | - | X | - | Pyrrhotite | Plagioclase albite |
| 64-477A | 64-477A-5-1,92-94 | 191.9 | X | - | XX | - | Q>>F | - | - | XX | - | - | - | - | X | - | Epidote | Plagioclase albite |
| 64-477A | 64-477A-5-1,114-120 | 192.1 | XX | - | XX | - | Q=F | - | - | XX | - | - | - | - | tr. | - | Some epidote | Plagioclase albite |
| 64-477A | 64-477A-6-CC,1-3 | 209.5 | XX | - | XX | - | Q=F | - | - | X | - | - | - | - | X | - | Plagioclase albite | |
| 64-477A | 64-477A-6-CC,4-6 | 209.5 | X | - | XX | - | Q>>F | - | - | XX | - | - | - | - | X | - | Plagioclase albite | |
| 64-477A | 64-477A-6-CC,114-120 | 200.6 | XX | - | X | - | Q<<F | - | - | XX | - | - | - | - | X | - | Some epidote | Plagioclase albite |
| 64-477A | 64-477A-7-1,50-52 | 210.5 | XX | - | XX | - | Q=F | - | - | X | - | - | - | - | X | - | Some epidote | Plagioclase albite |
| 64-477A | 64-477A-8-CC | 228.5 | XX | - | XX | - | Q=F | - | - | X | - | - | - | - | X | - | Epidote | Plagioclase albite |
| 64-477A | 64-477A-9-1,69-71 | 229.7 | XX | - | X | - | Q<F | - | - | X | - | - | - | - | X | - | Epidote | Plagioclase albite |
| 64-477A | 64-477A-9-1,84-86 | 229.8 | XX | - | XX | - | Q=F | - | - | X | - | - | - | - | X | - | Epidote | Plagioclase albite |
| 64-477A | 64-477A-10-1,110-120 | 239.6 | X | - | XX | - | Q>F | - | - | XX | - | - | - | - | X | - | Some pyrrhotite; epidote | Plagioclase albite |
| 64-477A | 64-477A-10-CC | 247.5 | XX | - | XX | - | Q<=F | - | - | X | - | - | - | - | - | - | Some epidote; pyrrhotite | Plagioclase albite |