Keigwin, Lloyd D; Rio, Domenico; Acton, Gary D; Shipboard Scientific Party (2005): Splice table (interval listing) of Site 172-1060 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.271639
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Keigwin, Lloyd D; Rio, Domenico; Acton, Gary D; et al. (1998): Proceedings of the Ocean Drilling Program 172 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 172, online, https://doi.org/10.2973/odp.proc.ir.172.1998
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 Earlier location no longer valid: http://mlp.ldeo.columbia.edu/BRG/ODP/ODP/CLIP/clip.html, http://www.odplegacy.org/PDF/Operations/Science/Lab_Procedures/Cookbooks/Downhole/CLIP_Cookbook.pdf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: 30.759694 * Longitude: -74.466500
Date/Time Start: 1997-03-05T00:00:00 * Date/Time End: 1997-03-05T00:00:00
Minimum Elevation: -3481.1 m * Maximum Elevation: -3481.1 m
Event(s):
172-1060 * Latitude: 30.759694 * Longitude: -74.466500 * Date/Time: 1997-03-05T00:00:00 * Elevation: -3481.1 m * Penetration: 426.5 m * Recovery: 442.8 m * Location: Blake-Bahama Outer Ridge, North Atlantic Ocean * Campaign: Leg172 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 46 cores; 426.5 m cored; 0 m drilled; 103.8% 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:
84 data points
Data
| 1 Event | 2 H | 3 MCD Top | 4 MCD Bot |
|---|---|---|---|
| 172-1060 | C | 0.1 | 6.86 |
| 172-1060 | A | 6.86 | 11.54 |
| 172-1060 | B | 11.54 | 19.18 |
| 172-1060 | A | 19.18 | 27.82 |
| 172-1060 | B | 27.82 | 30.46 |
| 172-1060 | C | 30.46 | 37.4 |
| 172-1060 | B | 37.5 | 45.9 |
| 172-1060 | C | 45.9 | 49.23 |
| 172-1060 | A | 49.23 | 56.71 |
| 172-1060 | B | 56.71 | 66.02 |
| 172-1060 | A | 66.02 | 71.49 |
| 172-1060 | B | 71.49 | 76.13 |
| 172-1060 | C | 76.13 | 82.61 |
| 172-1060 | A | 82.61 | 89.77 |
| 172-1060 | B | 89.77 | 96 |
| 172-1060 | C | 96 | 103.58 |
| 172-1060 | B | 103.58 | 110.62 |
| 172-1060 | C | 110.62 | 113.85 |
| 172-1060 | B | 113.85 | 122.01 |
| 172-1060 | A | 122.01 | 125.47 |
| 172-1060 | C | 125.47 | 128.21 |
| 172-1060 | A | 128.21 | 133.2 |
| 172-1060 | B | 133.2 | 141.11 |
| 172-1060 | A | 141.11 | 148.34 |
| 172-1060 | A | 148.34 | 153.23 |
| 172-1060 | A | 153.23 | 162.89 |
| 172-1060 | A | 162.89 | 172.27 |
| 172-1060 | A | 172.27 | 180.91 |