ARM and susceptibility record ans grain size distribution of ODP Hole 105-645C (Table 1)

DOI

The potential use of anhysteretic remanence/magnetic susceptibility (ARM/X) to indicate the relative grain-size variations of marine sediments is examined. Samples from Ocean Drilling Program (ODP) Hole 645C were measured for low-field magnetic susceptibility at two frequencies (0.47 and 4.7 kHz), given an anhysteretic remanence using a peak alternating magnetic (AC) field of 0.05 mT, and separated into the percentage sand, silt, and clay fractions. Results show little frequency dependence of low-field magnetic susceptibility and a direct relationship betweem ARM/X and clay concentration.

The values for ARM and susceptibility can be found in Hall and King (1989, dataset: doi:10.1594/PANGAEA.745265).

Supplement to: Hall, Frank R; Busch, William H; King, John W (1989): The relationship between variations in rock-magnetic properties and grain size of sediments from ODP Hole 645C. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 837-841

Identifier
DOI https://doi.org/10.1594/PANGAEA.745260
Related Identifier https://doi.org/10.2973/odp.proc.sr.105.149.1989
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.745260
Provenance
Creator Hall, Frank R; Busch, William H; King, John W
Publisher PANGAEA
Publication Year 1989
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 468 data points
Discipline Earth System Research
Spatial Coverage (-64.654 LON, 70.457 LAT); Baffin Bay
Temporal Coverage Begin 1985-09-10T01:25:00Z
Temporal Coverage End 1985-09-10T11:00:00Z