(Table 1) Magnetic properties of sediments at DSDP Holes 92-597B and 92-597C

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Autore principale: Nishitani, T
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1986
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author Nishitani, T
author_facet Nishitani, T
collection Datos científicos de ciencias marinas y ambientales
contents Measurements of magnetic properties were made on basalt samples recovered from Holes 597B and 597C. This paper describes the intensity and inclination of natural remanent magnetization (NRM), the intensity of anhysteretic remanent magnetization (ARM), the median demagnetizing field (MDF) for NRM and ARM, the initial susceptibility, the Koenigsberger ratio (Q). The mean inclinations (I) after alternating field demagnetization for Holes 597B and 597C are 45.4 ±7.1° and 45.0 ± 7.6°, respectively. These numeric quantities are greater than the calculated value of I = 34° expected at this site. A change of magnetic properties occurs at the depths of 100 and 120 m, respectively, which coincide with the boundaries between major petrological units.
format Dataset Open Access
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language en
publishDate 1986
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Magnetic properties of sediments at DSDP Holes 92-597B and 92-597C
Nishitani, T
92-597B; 92-597C; ARM, Intensity, per unit volume; ARM, median destructive field of anhysteretic remanent magnetization; Deep Sea Drilling Project; Demagnetizing field; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Inclination; Koenigsberger ratio; Leg92; NRM, Declination; NRM, Inclination; NRM, Intensity; NRM, Median destructive field of natural remanent magnetization; Piece; Sample code/label; South Pacific Ocean; Susceptibility; Susceptibility meter (Bison Model 3101)
Measurements of magnetic properties were made on basalt samples recovered from Holes 597B and 597C. This paper describes the intensity and inclination of natural remanent magnetization (NRM), the intensity of anhysteretic remanent magnetization (ARM), the median demagnetizing field (MDF) for NRM and ARM, the initial susceptibility, the Koenigsberger ratio (Q). The mean inclinations (I) after alternating field demagnetization for Holes 597B and 597C are 45.4 ±7.1° and 45.0 ± 7.6°, respectively. These numeric quantities are greater than the calculated value of I = 34° expected at this site. A change of magnetic properties occurs at the depths of 100 and 120 m, respectively, which coincide with the boundaries between major petrological units.
title (Table 1) Magnetic properties of sediments at DSDP Holes 92-597B and 92-597C
topic 92-597B; 92-597C; ARM, Intensity, per unit volume; ARM, median destructive field of anhysteretic remanent magnetization; Deep Sea Drilling Project; Demagnetizing field; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Inclination; Koenigsberger ratio; Leg92; NRM, Declination; NRM, Inclination; NRM, Intensity; NRM, Median destructive field of natural remanent magnetization; Piece; Sample code/label; South Pacific Ocean; Susceptibility; Susceptibility meter (Bison Model 3101)
url https://doi.org/10.1594/PANGAEA.792594