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Hamano, Yozo; Bina, M Mansour; Krammer, Kristian (1990): Paleomagnetism of serpentinized peridotites from ODP Hole 109-970A [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.745562, Supplement to: Hamano, Y et al. (1990): Paleomagnetism of the serpentinized peridotite from ODP Hole 670A. In: Detrick, R; Honnorez, J; Bryan, WB; Juteau, T; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 106/109, 257-262, https://doi.org/10.2973/odp.proc.sr.106109.152.1990

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Abstract:
Paleomagnetic studies on the serpentinized peridotites recovered from ODP Hole 670A were conducted in three laboratories. High NRM intensities and magnetic susceptibilities were observed in the serpentinized peridotites, which suggest that the remanent and the induced magnetizations of the peridotites cannot be neglected as a source of the magnetic anomalies observed at sea surface. The in situ low inclination of the magnetization indicated from the laboratory studies suggests that the peridotite body has been subjected to a large-scale deformation after the acquisition of the magnetization.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 23.166600 * Longitude: -45.032200
Date/Time Start: 1986-06-12T01:30:00 * Date/Time End: 1986-06-16T16:15:00
Event(s):
109-670A * Latitude: 23.166600 * Longitude: -45.032200 * Date/Time Start: 1986-06-12T01:30:00 * Date/Time End: 1986-06-16T16:15:00 * Elevation: -3625.0 m * Penetration: 92.5 m * Recovery: 4.58 m * Location: South Atlantic Ocean * Campaign: Leg109 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 7 cores; 76.6 m cored; 0 m drilled; 6 % recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2 datasets

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Datasets listed in this publication series

  1. Hamano, Y; Bina, MM; Krammer, K (1990): (Table 2) Inclinations and declination differences of oriented samples of ODP Hole 109-670A. https://doi.org/10.1594/PANGAEA.745561
  2. Hamano, Y; Bina, MM; Krammer, K (1990): (Table 1) NRM intensity, MDF, susceptibility and Q-ratio of serpentinized peridotites recovered from ODP Hole 109-670A. https://doi.org/10.1594/PANGAEA.745559