Dunn, Dean A; Patrick, David M; Cooley Jr, Ulysses (1987): (Table 5) Proportions of nonclay minerals at DSDP Holes 93-604 and 93-605 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.789085, In supplement to: Dunn, DA et al. (1987): Cenozoic clay mineralogy of Sites 604 and 605, New Jersey Transect, Deep Sea Drilling Project Leg 93. In: van Hinte, JE; Wise, SW Jr; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 93, 1023-1037, https://doi.org/10.2973/dsdp.proc.93.141.1987
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 38.727700 * Median Longitude: -72.579200 * South-bound Latitude: 38.713200 * West-bound Longitude: -72.609200 * North-bound Latitude: 38.742200 * East-bound Longitude: -72.549200
Date/Time Start: 1983-06-08T00:00:00 * Date/Time End: 1983-06-11T00:00:00
Minimum Elevation: -2361.0 m * Maximum Elevation: -2194.0 m
Event(s):
93-604 * Latitude: 38.713200 * Longitude: -72.549200 * Date/Time: 1983-06-08T00:00:00 * Elevation: -2361.0 m * Penetration: 294.5 m * Recovery: 118.6 m * Location: North Atlantic/CONT RISE * Campaign: Leg93 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 275.3 m cored; 19.2 m drilled; 43.1 % recovery
93-605 * Latitude: 38.742200 * Longitude: -72.609200 * Date/Time: 1983-06-11T00:00:00 * Elevation: -2194.0 m * Penetration: 816.7 m * Recovery: 532 m * Location: North Atlantic * Campaign: Leg93 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 69 cores; 652.8 m cored; 9.6 m drilled; 81.5 % recovery
Comment:
#0 = present, but not quantified
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Dunn, Dean A | DSDP/ODP/IODP sample designation | ||
| 3 | Epoch | Epoch | Dunn, Dean A | |||
| 4 | Quartz | Qz | % | Dunn, Dean A | ||
| 5 | Calcite | Cal | % | Dunn, Dean A | ||
| 6 | Feldspar | Fsp | % | Dunn, Dean A | ||
| 7 | Siderite | Sd | % | Dunn, Dean A | ||
| 8 | Glauconite | Glt | % | Dunn, Dean A | ||
| 9 | Cristobalite | Crs | % | Dunn, Dean A | ||
| 10 | Amphibole | Amp | % | Dunn, Dean A |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
198 data points
Data
| 1 Event | 2 Sample label | 3 Epoch | 4 Qz [%] | 5 Cal [%] | 6 Fsp [%] | 7 Sd [%] | 8 Glt [%] | 9 Crs [%] | 10 Amp [%] |
|---|---|---|---|---|---|---|---|---|---|
| 93-604 | 93-604-1-1,130 | late Pleistocene | 81 | 7 | 12 | 0 | 0 | 0 | #0 |
| 93-604 | 93-604-10-4,100 | early Pleistocene | 100 | 0 | 31 | 0 | 0 | 0 | 0 |
| 93-604 | 93-604-13-1,106 | early Pleistocene | 55 | 14 | 14 | 0 | 0 | 0 | 0 |
| 93-604 | 93-604-16-4,100 | late Pliocene | 80 | 6 | 10 | 0 | 0 | 0 | #0 |
| 93-604 | 93-604-18-4,100 | late Pliocene | 77 | 13 | 0 | 0 | 0 | 0 | 0 |
| 93-604 | 93-604-22-2,100 | early Pliocene | 70 | 30 | 0 | 0 | 0 | 0 | 0 |
| 93-604 | 93-604-25-4,100 | early Pliocene | 100 | 0 | 0 | 0 | 0 | 0 | 0 |
| 93-604 | 93-604-27-1,140 | late Miocene | 100 | 0 | 0 | 0 | 0 | 0 | 0 |
| 93-604 | 93-604-6-3,130 | late Pleistocene | 48 | 21 | 31 | 0 | 0 | 0 | #0 |
| 93-604 | 93-604-8-2,57 | late Pleistocene | 73 | 12 | 15 | 0 | 0 | 0 | 0 |
| 93-605 | 93-605-1-1,100 | middle Pleistocene | 100 | 0 | 0 | 0 | 0 | 0 | 0 |
| 93-605 | 93-605-15-2,100 | middle Eocene | 0 | 100 | 0 | 0 | 0 | #0 | 0 |
| 93-605 | 93-605-21-3,100 | middle Eocene | 0 | 100 | 0 | 0 | 0 | #0 | 0 |
| 93-605 | 93-605-27-1,100 | early Eocene | 0 | 90 | 0 | 10 | 0 | #0 | 0 |
| 93-605 | 93-605-33-5,100 | early Eocene | 14 | 86 | 0 | 0 | 0 | #0 | 0 |
| 93-605 | 93-605-4-3,100 | middle Pleistocene | 57 | 16 | 26 | 0 | #0 | #0 | #0 |
| 93-605 | 93-605-40-2,100 | early Eocene | 32 | 68 | 0 | 0 | 0 | #0 | 0 |
| 93-605 | 93-605-48-4,100 | late Paleocene | 45 | 55 | 0 | 0 | 0 | 0 | #0 |
| 93-605 | 93-605-54-1,100 | late Paleocene | 39 | 61 | 0 | 0 | 0 | #0 | 0 |
| 93-605 | 93-605-59-4,100 | early Paleocene | 42 | 58 | 0 | 0 | 0 | #0 | 0 |
| 93-605 | 93-605-64-3,100 | early Paleocene | 57 | 43 | 0 | 0 | 0 | 0 | 0 |
| 93-605 | 93-605-7-6,100 | middle Eocene | 0 | 100 | 0 | 0 | #0 | 0 | 0 |