Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East Antarctica

Natural remanent magnetizations (NRMs) of 5 dirt-ice layers including tephra collected from the Allan Hills in Southern Victoria Land, the Yamato Mountains and the Sφr Rondane Mountains in Eastern Queen Maud Land, East Antarctica, were investigated. The NRMs with 1.38 to 22.1×(10)^<-7>Am^2/kg...

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Main Author: Minoru Funaki
Format: Article
Language:English
Published: National Institute of Polar Research 1990-07-01
Series:Antarctic Record
Online Access:https://doi.org/10.15094/00008672
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author Minoru Funaki
author_facet Minoru Funaki
author_sort Minoru Funaki
collection DOAJ
description Natural remanent magnetizations (NRMs) of 5 dirt-ice layers including tephra collected from the Allan Hills in Southern Victoria Land, the Yamato Mountains and the Sφr Rondane Mountains in Eastern Queen Maud Land, East Antarctica, were investigated. The NRMs with 1.38 to 22.1×(10)^<-7>Am^2/kg in intensity were very stable against AF demagnetization at least up to 50mT. The magnetic layers consisted with the dirt-ice layers recognized by the naked eye, but magnetizations in the clear-ice were weak for any significant measurements. The uniform NRM directions were obtained in the dirt-ice layers with upward directions. Those of the oriented 2 samples (A, E) were almost parallel to the present geomagnetic field direction in situ. So, a possible mechanism is rearrangement of the magnetic grains adjusting the NRM directions to the geomagnetic field direction due to partial melting of the ice around the grains by the solar radiation.
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spelling doaj.art-388261e0680140b89321165f986418682022-12-21T22:26:08ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1990-07-0134213013810.15094/00008672Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East AntarcticaMinoru Funaki0National Institute of Polar ResearchNatural remanent magnetizations (NRMs) of 5 dirt-ice layers including tephra collected from the Allan Hills in Southern Victoria Land, the Yamato Mountains and the Sφr Rondane Mountains in Eastern Queen Maud Land, East Antarctica, were investigated. The NRMs with 1.38 to 22.1×(10)^<-7>Am^2/kg in intensity were very stable against AF demagnetization at least up to 50mT. The magnetic layers consisted with the dirt-ice layers recognized by the naked eye, but magnetizations in the clear-ice were weak for any significant measurements. The uniform NRM directions were obtained in the dirt-ice layers with upward directions. Those of the oriented 2 samples (A, E) were almost parallel to the present geomagnetic field direction in situ. So, a possible mechanism is rearrangement of the magnetic grains adjusting the NRM directions to the geomagnetic field direction due to partial melting of the ice around the grains by the solar radiation.https://doi.org/10.15094/00008672
spellingShingle Minoru Funaki
Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East Antarctica
Antarctic Record
title Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East Antarctica
title_full Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East Antarctica
title_fullStr Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East Antarctica
title_full_unstemmed Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East Antarctica
title_short Note on the natural remanent magnetizations of dirt-ice layers collected from the bare ice field in East Antarctica
title_sort note on the natural remanent magnetizations of dirt ice layers collected from the bare ice field in east antarctica
url https://doi.org/10.15094/00008672
work_keys_str_mv AT minorufunaki noteonthenaturalremanentmagnetizationsofdirticelayerscollectedfromthebareicefieldineastantarctica