Odin, G S; Stephan, J F (1982): (Table 4) K-Ar data on glauconites and clay fraction of sediments at DSDP Leg 66 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817578, In supplement to: Odin, GS; Stephan, JF (1982): The occurrence of deep water glaucony from the Eastern Pacific: The result of in situ genesis or subsidence? In: Watkins, JS; Casey Moore, J; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 66, 419-428, https://doi.org/10.2973/dsdp.proc.66.110.1982
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 16.169300 * Median Longitude: -99.006867 * South-bound Latitude: 16.078800 * West-bound Longitude: -99.056500 * North-bound Latitude: 16.269800 * East-bound Longitude: -98.945300
Date/Time Start: 1979-04-03T00:00:00 * Date/Time End: 1979-04-20T00:00:00
Minimum Elevation: -1935.0 m * Maximum Elevation: -1240.0 m
Event(s):
66-489 * Latitude: 16.269800 * Longitude: -99.018800 * Date/Time: 1979-04-03T00:00:00 * Elevation: -1240.0 m * Penetration: 53.5 m * Recovery: 23.1 m * Location: North Pacific/TRENCH * Campaign: Leg66 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 44 m cored; 0 m drilled; 52.6 % recovery
66-490 * Latitude: 16.159300 * Longitude: -99.056500 * Date/Time: 1979-04-08T00:00:00 * Elevation: -1761.0 m * Penetration: 588.5 m * Recovery: 343.4 m * Location: North Pacific/TRANSITION ZONE * Campaign: Leg66 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 63 cores; 577 m cored; 9 m drilled; 59.5 % recovery
66-492A * Latitude: 16.078800 * Longitude: -98.945300 * Date/Time: 1979-04-20T00:00:00 * Elevation: -1935.0 m * Penetration: 70.8 m * Recovery: 28.3 m * Location: North Pacific/SLOPE * Campaign: Leg66 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 51.8 m cored; 0 m drilled; 54.6 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Sample code/label | Sample label | Odin, G S | DSDP/ODP/IODP sample designation | ||
| 6 | Description | Description | Odin, G S | A = grain size 0.16-0.50 mm (generally the main fraction); H = attractable at 0.45 Å at the magnetic separaton | ||
| 7 | Potassium | K | % | Odin, G S | Analyses were done by M. Lenoble; Argon analyses were done by M. G. Bonhomme, Université de Strasbourg | |
| 8 | Sample method | Sample method | Odin, G S | |||
| 9 | Argon-40, radiogenic/Argon-40, total | 40Ar*/40Ar(tot) | Odin, G S | |||
| 10 | Argon-40 | 40Ar | nl/g | Odin, G S | Radiogenic | |
| 11 | Age, dated | Age dated | ka | Odin, G S | The apparent age of the detrital clay fraction is inherited and is probably similar to that of the initial substrate of glauconitization. The apparent ages of the glauconies demonstrate once more the presence of part of the initial radiogenic argon as it might have been foreseen from their level of evolution. The apparent ages cannot be related to the epoch of genesis. | |
| 12 | Age, dated standard deviation | Age dated std dev | ± | Odin, G S |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
51 data points