Ogg, James G; Kodama, Kazuto; Wallick, Brian P (1992): (Appendix 2) Magnetic polarity and characteristic directions of DSDP Hole 27-261 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.762801, In supplement to: Ogg, JG et al. (1992): Lower Cretaceous magnetostratigraphy and paleolatitudes off Northwest Australia, ODP Site 765 and DSDP Site 261, Argo Abyssal Plain, and ODP Site 766, Gascoyne Abyssal Plain. In: Gradstein, FM; Ludden, JN; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 123, 523-548, https://doi.org/10.2973/odp.proc.sr.123.128.1992
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -12.947200 * Longitude: 117.892700
Date/Time Start: 1972-11-17T00:00:00 * Date/Time End: 1972-11-17T00:00:00
Minimum DEPTH, sediment/rock: 332.94 m * Maximum DEPTH, sediment/rock: 535.58 m
Event(s):
27-261 * Latitude: -12.947200 * Longitude: 117.892700 * Date/Time: 1972-11-17T00:00:00 * Elevation: -5667.0 m * Penetration: 579.5 m * Recovery: 120.5 m * Location: Indian Ocean//PLAIN * Campaign: Leg27 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 36 cores; 323 m cored; 9.5 m drilled; 37.3 % recovery
Comment:
Sediment depth is given in mbsf. Characteristic directions and mean intensities are computed from least-squares analysis of the indicated suites of selected demagnetization steps. Selected steps are thermal demagnetization levels for. Org indicates that the origin of the vector plot was included as a selected point for the least-squares computation due to irregular pattern of demagnetization vectors; Tied indicates that the least-squares vector was constrained to pass through the origin on the vector plots, thereby producing an average of the selected demagnetization steps - such Org and Tied computations are given a lower quality rating.
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
620 data points