Jansen, Eystein; Blum, Peter; Shipboard Scientific Party (2005): Splice table (interval listing) of Site 162-985 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.271618
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Jansen, Eystein; Raymo, Maureen E; Blum, Peter; et al. (1996): Proceedings of the Ocean Drilling Program, 162 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 162, https://doi.org/10.2973/odp.proc.ir.162.1996
ODP/TAMU (2005): JANUS Database. Ocean Drilling Program, Texas A&M University, College Station TX 77845-9547, USA; (data copied from Janus 2005-02 to 2005-06), http://www-odp.tamu.edu/database/
Further details:
ODP Core Log integration platform. Earlier location no longer valid: http://mlp.ldeo.columbia.edu/BRG/ODP/ODP/CLIP/clip.html, http://www.odplegacy.org/PDF/Operations/Science/Lab_Procedures/Cookbooks/Downhole/CLIP_Cookbook.pdf
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 66.941550 * Longitude: -6.450150
Date/Time Start: 1995-08-03T00:00:00 * Date/Time End: 1995-08-07T00:00:00
Minimum Elevation: -2833.5 m * Maximum Elevation: -2833.5 m
Event(s):
162-985 * Latitude: 66.941550 * Longitude: -6.450150 * Date/Time Start: 1995-08-03T00:00:00 * Date/Time End: 1995-08-07T00:00:00 * Elevation: -2833.5 m * Penetration: 714.8 m * Recovery: 682.9 m * Location: Norwegian Sea * Campaign: Leg162 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 76 cores; 714.8 m cored; 0 m drilled; 95.5% recovery
Comment:
Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
78 data points
Data
| 1 Event | 2 H | 3 MCD Top | 4 MCD Bot |
|---|---|---|---|
| 162-985 | A | 0.22 | 1.58 |
| 162-985 | B | 1.58 | 7.08 |
| 162-985 | A | 7.08 | 12.12 |
| 162-985 | A | 12.12 | 18.42 |
| 162-985 | B | 18.41 | 27.18 |
| 162-985 | A | 27.18 | 28.63 |
| 162-985 | B | 28.63 | 36.46 |
| 162-985 | A | 36.46 | 38.71 |
| 162-985 | B | 38.71 | 46.62 |
| 162-985 | A | 46.62 | 50.01 |
| 162-985 | B | 50.01 | 55.89 |
| 162-985 | A | 55.89 | 61.41 |
| 162-985 | B | 61.41 | 68.33 |
| 162-985 | A | 68.33 | 73.95 |
| 162-985 | B | 73.95 | 78.09 |
| 162-985 | A | 78.09 | 81.38 |
| 162-985 | B | 81.38 | 87.77 |
| 162-985 | A | 87.77 | 94.89 |
| 162-985 | B | 94.89 | 96.78 |
| 162-985 | A | 96.78 | 102.65 |
| 162-985 | B | 102.65 | 107.56 |
| 162-985 | A | 107.56 | 114.67 |
| 162-985 | B | 114.67 | 118.63 |
| 162-985 | A | 118.63 | 125.58 |
| 162-985 | B | 125.58 | 127.47 |
| 162-985 | A | 127.47 | 134.52 |