Chamley, Hervè; Coulon, Hervé; Debrabant, Pierre; Holtzapffel, Thierry (1986): (Table 2) Bulk mineralogy at DSDP Site 89-585 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.793282, In supplement to: Chamley, H et al. (1986): Cretaceous interactions between volcanism and sedimentation in the East Mariana Basin, from mineralogical, micromorphological, and geochemical investigations, Deep Sea Drilling Project Site 585. In: Moberly, R; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 89, 413-429, https://doi.org/10.2973/dsdp.proc.89.113.1986
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 13.483300 * Longitude: 156.815200
Date/Time Start: 1982-10-18T00:00:00 * Date/Time End: 1982-10-18T00:00:00
Minimum Elevation: -6109.0 m * Maximum Elevation: -6109.0 m
Event(s):
89-585 * Latitude: 13.483300 * Longitude: 156.815200 * Date/Time: 1982-10-18T00:00:00 * Elevation: -6109.0 m * Penetration: 763.7 m * Recovery: 165.2 m * Location: North Pacific/BASIN * Campaign: Leg89 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 54 cores; 505.5 m cored; 9.1 m drilled; 32.7 % recovery
89-585A * Latitude: 13.483300 * Longitude: 156.815200 * Date/Time: 1982-10-18T00:00:00 * Elevation: -6109.0 m * Penetration: 892.8 m * Recovery: 101.5 m * Location: North Pacific/BASIN * Campaign: Leg89 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 22 cores; 208.8 m cored; 0 m drilled; 48.6 % recovery
Comment:
The abundance of each mineral is given by the height of the major peak (I 100) above the background of the powder X-ray diffraction diagrams, according to a conventional scale: very abundant (VA = > 150 mm), abundant (A = 40-150 mm), common (AR = 10-40 mm), rare (R = 4-10 mm), very rare (VR = <4 mm), - = absent.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Sample code/label | Sample label | Chamley, Hervè | DSDP/ODP/IODP sample designation | ||
3 | Quartz | Qz | Chamley, Hervè | X-ray diffraction (XRD) | ||
4 | Feldspar | Fsp | Chamley, Hervè | X-ray diffraction (XRD) | ||
5 | Clay | Clay | Chamley, Hervè | X-ray diffraction (XRD) | ||
6 | Pyrite | Py | Chamley, Hervè | X-ray diffraction (XRD) | ||
7 | Calcite | Cal | Chamley, Hervè | X-ray diffraction (XRD) | ||
8 | Opal-CT | Opal-CT | Chamley, Hervè | X-ray diffraction (XRD) | ||
9 | Clinoptilolite | Cpt | Chamley, Hervè | X-ray diffraction (XRD) | ||
10 | Analcite | Anl | Chamley, Hervè | X-ray diffraction (XRD) | ||
11 | Celadonite | Cel | Chamley, Hervè | X-ray diffraction (XRD) | ||
12 | Augite | Aug | Chamley, Hervè | X-ray diffraction (XRD) | ||
13 | Olivine | Ol | Chamley, Hervè | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
480 data points
Data
1 Event | 2 Sample label | 3 Qz | 4 Fsp | 5 Clay | 6 Py | 7 Cal | 8 Opal-CT | 9 Cpt | 10 Anl | 11 Cel | 12 Aug | 13 Ol |
---|---|---|---|---|---|---|---|---|---|---|---|---|
89-585 | 89-585-17-2,146 | VR | - | AR | - | VA | R | VR | - | - | - | - |
89-585 | 89-585-18-1,50 | VR | VR | R | - | VA | VA | VR | - | - | - | - |
89-585 | 89-585-19-1,15 | A | - | A | R | - | - | AR | - | - | - | - |
89-585 | 89-585-20-2,101 | AR | - | A | R | - | - | AR | - | - | - | - |
89-585 | 89-585-26-1,26 | R | - | A | - | - | VA | R | - | - | - | - |
89-585 | 89-585-26-1,63 | - | A | A | - | - | - | R | - | - | - | - |
89-585 | 89-585-27-1,13 | - | A | A | - | - | - | VR | - | - | - | - |
89-585 | 89-585-27-4,57 | R | R | AR | - | - | VA | AR | - | - | - | - |
89-585 | 89-585-27-4,74 | R | - | AR | - | - | VA | AR | - | - | - | - |
89-585 | 89-585-28-4,30 | AR | - | A | - | R | A | R | - | - | - | - |
89-585 | 89-585-29-2,63 | AR | R | A | - | VR | A | VR | - | - | - | - |
89-585 | 89-585-30-1,50 | AR | - | A | - | AR | A | VR | - | - | - | - |
89-585 | 89-585-31-3,29 | AR | R | VA | - | R | - | R | - | - | - | - |
89-585 | 89-585-34-2,85 | VA | - | AR | - | AR | - | - | - | - | - | - |
89-585 | 89-585-35-1,1 | AR | R | A | - | AR | R | - | - | - | - | - |
89-585 | 89-585-37-1,31 | VA | - | R | - | - | A | - | - | - | - | - |
89-585 | 89-585-38-1,9 | A | AR | A | - | - | - | - | - | - | - | - |
89-585 | 89-585-39-1,132 | A | VR | VA | - | R | - | R | - | - | - | - |
89-585 | 89-585-43-1,13 | VR | R | VA | - | R | - | - | - | - | R | - |
89-585 | 89-585-44-3,17 | R | AR | A | - | R | - | - | - | - | AR | - |
89-585 | 89-585-45-1,8 | R | R | VA | - | R | - | - | - | - | - | - |
89-585 | 89-585-46-2,40 | R | AR | A | - | AR | - | - | AR | - | AR | - |
89-585 | 89-585-48-2,4 | R | AR | AR | - | AR | - | - | A | AR | AR | - |
89-585 | 89-585-49-5,117 | - | AR | A | - | - | - | R | - | - | AR | - |
89-585 | 89-585-54-3,11 | - | - | AR | - | R | - | - | A | AR | R | AR |
89-585 | 89-585-55-1,11 | - | - | AR | - | - | - | - | - | AR | R | - |
89-585A | 89-585A-5-1,79 | VR | R | AR | - | - | VA | VR | - | - | - | - |
89-585A | 89-585A-5-3,13 | AR | R | A | - | R | A | VR | - | - | - | - |
89-585A | 89-585A-7-1,92 | AR | R | A | - | - | R | - | - | - | - | - |
89-585A | 89-585A-7-3,70 | A | R | A | - | - | AR | R | - | - | - | - |
89-585A | 89-585A-8-1,7 | - | A | A | - | - | R | R | - | - | - | - |
89-585A | 89-585A-9-1,67 | - | AR | AR | - | R | A | - | - | - | - | - |
89-585A | 89-585A-10-1,1 | A | VR | AR | - | R | - | - | - | - | - | - |
89-585A | 89-585A-11-1,113 | VA | - | R | - | - | - | - | A | R | AR | - |
89-585A | 89-585A-12-4,61 | - | - | AR | - | - | - | - | A | R | AR | AR |
89-585A | 89-585A-12-CC | - | - | AR | - | - | - | - | A | AR | A | - |
89-585A | 89-585A-15-5,137 | - | R | R | - | R | - | - | A | - | AR | - |
89-585A | 89-585A-16-1,6 | - | R | AR | - | - | - | - | A | AR | AR | - |
89-585A | 89-585A-17-1,15 | - | R | A | - | R | - | - | A | R | R | - |
89-585A | 89-585A-18-2,1 | - | R | A | - | - | - | - | A | R | AR | - |