ARM and susceptibility record ans grain size distribution of ODP Hole 105-645C (Table 1)
Hall, Frank R;Busch, William H;King, John W
Description
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.
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Metrics Over Time
Publication Details
Subfield
Mechanics of Materials
Field
Engineering
Domain
Physical Sciences
Confidence Score
39%
Source
Scholar Data Model
Keywords
Sample code/labelDEPTH, sediment/rockSandSiltSize fraction < 0.002 mm, clayARM, Susceptibility/susceptibilityRatioDrilling/drill rigDSDP/ODP/IODP sample designationGravimetric analysisLeg105Joides ResolutionOcean Drilling Program (ODP)