NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)

The remanence properties of 62 cement samples from Cores 7R, 11R, and 12R recovered from Hole 648B were examined. The remanent magnetization consists of two components, where the soft component is carried by the basalt fragments in the cement sample and the hard component is carried by fine magnetic...

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Bibliographic Details
Main Authors: Hamano, Yozo, Ohno, Masao
Format: Dataset
Language:English
Published: PANGAEA 1990
Subjects:
109-648B
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Joides Resolution
Leg109
North Atlantic Ocean
NRM
Inclination
Intensity
Median destructive field of natural remanent magnetization
Ocean Drilling Program
ODP
Sample code/label
Susceptibility
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.745566
https://doi.org/10.1594/PANGAEA.745566
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.745566
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.745566 2024-09-15T18:23:22+00:00 NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1) Hamano, Yozo Ohno, Masao LATITUDE: 22.922000 * LONGITUDE: -44.947100 * DATE/TIME START: 1986-04-29T04:00:00 * DATE/TIME END: 1986-05-31T04:30:00 * MINIMUM DEPTH, sediment/rock: 14.92 m * MAXIMUM DEPTH, sediment/rock: 19.54 m 1990 text/tab-separated-values, 310 data points https://doi.pangaea.de/10.1594/PANGAEA.745566 https://doi.org/10.1594/PANGAEA.745566 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.745566 https://doi.org/10.1594/PANGAEA.745566 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Hamano, Yozo; Ohno, Masao (1990): Remanent magnetization of cement cores from Hole 648B: a possible logging tool for the downhole measurements of magnetic field. 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, 275-281, https://doi.org/10.2973/odp.proc.sr.106109.155.1990 109-648B DEPTH sediment/rock DRILL Drilling/drill rig DSDP/ODP/IODP sample designation Joides Resolution Leg109 North Atlantic Ocean NRM Inclination Intensity Median destructive field of natural remanent magnetization Ocean Drilling Program ODP Sample code/label Susceptibility dataset 1990 ftpangaea https://doi.org/10.1594/PANGAEA.74556610.2973/odp.proc.sr.106109.155.1990 2024-08-21T00:02:26Z The remanence properties of 62 cement samples from Cores 7R, 11R, and 12R recovered from Hole 648B were examined. The remanent magnetization consists of two components, where the soft component is carried by the basalt fragments in the cement sample and the hard component is carried by fine magnetic grains originally contained in cement. The hard component was used to estimate the variation of the magnetic field inclination within the hole. The result indicates that some parts of the basalt section within the sub-bottom depth between 15 and 20 m are reversely magnetized, which can be attributed to the displacement of pillow basalt after its solidification. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-44.947100,-44.947100,22.922000,22.922000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 109-648B
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Joides Resolution
Leg109
North Atlantic Ocean
NRM
Inclination
Intensity
Median destructive field of natural remanent magnetization
Ocean Drilling Program
ODP
Sample code/label
Susceptibility
spellingShingle 109-648B
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Joides Resolution
Leg109
North Atlantic Ocean
NRM
Inclination
Intensity
Median destructive field of natural remanent magnetization
Ocean Drilling Program
ODP
Sample code/label
Susceptibility
Hamano, Yozo
Ohno, Masao
NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)
topic_facet 109-648B
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP/ODP/IODP sample designation
Joides Resolution
Leg109
North Atlantic Ocean
NRM
Inclination
Intensity
Median destructive field of natural remanent magnetization
Ocean Drilling Program
ODP
Sample code/label
Susceptibility
description The remanence properties of 62 cement samples from Cores 7R, 11R, and 12R recovered from Hole 648B were examined. The remanent magnetization consists of two components, where the soft component is carried by the basalt fragments in the cement sample and the hard component is carried by fine magnetic grains originally contained in cement. The hard component was used to estimate the variation of the magnetic field inclination within the hole. The result indicates that some parts of the basalt section within the sub-bottom depth between 15 and 20 m are reversely magnetized, which can be attributed to the displacement of pillow basalt after its solidification.
format Dataset
author Hamano, Yozo
Ohno, Masao
author_facet Hamano, Yozo
Ohno, Masao
author_sort Hamano, Yozo
title NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)
title_short NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)
title_full NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)
title_fullStr NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)
title_full_unstemmed NRM intensity, MDF, stable inclination and susceptibility of cement samples of ODP Hole 109-648B (Table 1)
title_sort nrm intensity, mdf, stable inclination and susceptibility of cement samples of odp hole 109-648b (table 1)
publisher PANGAEA
publishDate 1990
url https://doi.pangaea.de/10.1594/PANGAEA.745566
https://doi.org/10.1594/PANGAEA.745566
op_coverage LATITUDE: 22.922000 * LONGITUDE: -44.947100 * DATE/TIME START: 1986-04-29T04:00:00 * DATE/TIME END: 1986-05-31T04:30:00 * MINIMUM DEPTH, sediment/rock: 14.92 m * MAXIMUM DEPTH, sediment/rock: 19.54 m
long_lat ENVELOPE(-44.947100,-44.947100,22.922000,22.922000)
genre North Atlantic
genre_facet North Atlantic
op_source Supplement to: Hamano, Yozo; Ohno, Masao (1990): Remanent magnetization of cement cores from Hole 648B: a possible logging tool for the downhole measurements of magnetic field. 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, 275-281, https://doi.org/10.2973/odp.proc.sr.106109.155.1990
op_relation https://doi.pangaea.de/10.1594/PANGAEA.745566
https://doi.org/10.1594/PANGAEA.745566
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.74556610.2973/odp.proc.sr.106109.155.1990
_version_ 1810463564960366592

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