Roperch, Pierrick; Chabernaud, Thierry; Calza, Francoise (1994): (Table 1) Anisotropy of magnetic susceptibility parameters of ODP Hole 134-833B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.787641, Supplement to: Roperch, P et al. (1994): Magnetic properties of a volcanic-rich sedimentary sequence in the intra-Arc Aoba Basin. In: Green, HG; Collot, J-Y; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 134, 491-507, https://doi.org/10.2973/odp.proc.sr.134.027.1994
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Abstract:
Ocean Drilling Program (ODP) Sites 832 and 833 were drilled in the intra-arc North Aoba Basin of the New Hebrides Island Arc (Vanuatu). High volcanic influxes in the intra-arc basin sediment resulting from erosion of volcanic rocks from nearby islands and from volcanic activity are associated with characteristic magnetic signals. The high magnetic susceptibility in the sediment (varying on average from 0.005 to more than 0.03 SI) is one of the most characteristic physical properties of this sedimentary depositional environment because of the high concentration of magnetites in redeposited ash flows and in coarse-grained turbidites.
Susceptibility data correlate well with the high resolution electrical resistivity logs recorded by the formation microscanner (FMS) tool. Unlike the standard geophysical logs, which have low vertical resolution and therefore smooth the record of the sedimentary process, the FMS and whole-core susceptibility data provide a clearer picture of turbiditic sediment deposition.
Measurements of Curie temperatures and low-temperature susceptibility behavior indicate that the principal magnetic minerals in ash beds, silt, and volcanic sandstone are Ti-poor titanomagnetite, whereas Ti-rich titanomagnetites are found in the intrusive sills at the bottom of Site 833. Apart from an increase in the concentration of magnetite in the sandstone layer, acquisition of isothermal and anhysteretic remanences does not show significant differences between sandstone and clayey silts. The determination of the anisotropy of magnetic susceptibility (AMS) in more than 400 samples show that clayey siltstone have a magnetic anisotropy up to 15%, whereas the AMS is much reduced in sandstone layers. The magnetic susceptibility fabric is dominated by the foliation plane, which is coplanar to the bedding plane. Reorientations of the samples using characteristic remanent magnetizations indicate that the bedding planes dip about 10° toward the east, in agreement with results from FMS images.
Basaltic sills drilled at Site 833 have high magnetic susceptibilities (0.05 to 0.1 SI) and strong remanent magnetizations. Magnetic field anomalies up to 50 µT were measured in the sills by the general purpose inclinometer tool (GPIT). The direction of the in-situ magnetic anomaly vectors, calculated from the GPIT, is oriented toward the southeast with shallow inclinations which suggests that the sill intruded during a reversed polarity period.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -14.876000 * Longitude: 167.880000
Date/Time Start: 1990-12-03T10:30:00 * Date/Time End: 1990-12-14T00:30:00
Minimum Elevation: -2640.0 m * Maximum Elevation: -2640.0 m
Event(s):
134-833B * Latitude: -14.876000 * Longitude: 167.880000 * Date/Time Start: 1990-12-03T10:30:00 * Date/Time End: 1990-12-14T00:30:00 * Elevation: -2640.0 m * Penetration: 1001.1 m * Recovery: 519.54 m * Location: Coral Sea * Campaign: Leg134 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 99 cores; 923.7 m cored; 0 m drilled; 56.2 % recovery
Comment:
Samples of interval 134-833B-83R to 134-833B-91R from basaltic sills, of interval 134-833B-94R to 134-833B-89R from sediments interlayerd with the sills.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Roperch, Pierrick | DSDP/ODP/IODP sample designation | ||
| 2 | Sample code/label 2 | Sample label 2 | Roperch, Pierrick | |||
| 3 | Sample amount | N | # | Roperch, Pierrick | ||
| 4 | Principle axes K1 of normalized anisotropy tensor | K max | Roperch, Pierrick | |||
| 5 | Declination of principle axis K1 | D(Kmax) | deg | Roperch, Pierrick | ||
| 6 | Inclination of principle axis K1 | I(Kmax) | deg | Roperch, Pierrick | ||
| 7 | Principle axes K2 of normalized anisotropy tensor | K int | Roperch, Pierrick | |||
| 8 | Declination of principle axis K2 | D(Kint) | deg | Roperch, Pierrick | ||
| 9 | Inclination of principle axis K2 | I(Kint) | deg | Roperch, Pierrick | ||
| 10 | Principle axes K3 of normalized anisotropy tensor | K min | Roperch, Pierrick | |||
| 11 | Declination of principle axis K3 | D(Kmin) | deg | Roperch, Pierrick | ||
| 12 | Inclination of principle axis K3 | I(Kmin) | deg | Roperch, Pierrick | ||
| 13 | Anisotropy-magnetic susceptibility, factor L, lineation | AMS factor L | Roperch, Pierrick | K max/K int | ||
| 14 | Anisotropy-magnetic susceptibility, factor F, foliation | AMS factor F | Roperch, Pierrick | K int/K min | ||
| 15 | Anisotropy-magnetic susceptibility, factor P, anisotropy degree | AMS factor P | Roperch, Pierrick | K max/K min [%] |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
135 data points