Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determination

Thirteen samples of volcanic rocks from Caucasus, Iceland and Philippines were subjected to low-temperature treatment in order to remove the part of remanent magnetization carried by multi-domain grains. Ten to 40% of multi-domain partial thermoremanence were removed, which may help to increase the...

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Main Authors: Ana-María Soler, Luis Alva-Valdivia, Avto Goguitchaichvili, Juan Morales
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geofísica 2001-08-01
Series:Geofísica Internacional
Subjects:
Online Access:http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2001/04/morales.pdf
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author Ana-María Soler
Luis Alva-Valdivia
Avto Goguitchaichvili
Juan Morales
author_facet Ana-María Soler
Luis Alva-Valdivia
Avto Goguitchaichvili
Juan Morales
author_sort Ana-María Soler
collection DOAJ
description Thirteen samples of volcanic rocks from Caucasus, Iceland and Philippines were subjected to low-temperature treatment in order to remove the part of remanent magnetization carried by multi-domain grains. Ten to 40% of multi-domain partial thermoremanence were removed, which may help to increase the success of paleointensity experiments. A sample from the 1991 eruption of Pinatubo volcano shows a total self-reversal due to ilmeno-hematites and partial self-reversal between 500° and 575 °C due to titano-magnetites. Low temperature demagnetization applied to self-reversed remanence suggest that the high-temperature peak is almost suppressed by this treatment.
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spelling doaj.art-9251960b26cb4047a597112ef40be8ab2023-09-02T09:38:23ZengUniversidad Nacional Autónoma de México, Instituto de GeofísicaGeofísica Internacional0016-71692001-08-01404293300Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determinationAna-María SolerLuis Alva-ValdiviaAvto GoguitchaichviliJuan MoralesThirteen samples of volcanic rocks from Caucasus, Iceland and Philippines were subjected to low-temperature treatment in order to remove the part of remanent magnetization carried by multi-domain grains. Ten to 40% of multi-domain partial thermoremanence were removed, which may help to increase the success of paleointensity experiments. A sample from the 1991 eruption of Pinatubo volcano shows a total self-reversal due to ilmeno-hematites and partial self-reversal between 500° and 575 °C due to titano-magnetites. Low temperature demagnetization applied to self-reversed remanence suggest that the high-temperature peak is almost suppressed by this treatment.http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2001/04/morales.pdfRock-magnetismlow-temperature demagnetizationdomain structure
spellingShingle Ana-María Soler
Luis Alva-Valdivia
Avto Goguitchaichvili
Juan Morales
Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determination
Geofísica Internacional
Rock-magnetism
low-temperature demagnetization
domain structure
title Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determination
title_full Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determination
title_fullStr Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determination
title_full_unstemmed Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determination
title_short Low-temperature demagnetization of volcanic rocks containing multi-domain magnetic grains: Implications for the Thellier paleointensity determination
title_sort low temperature demagnetization of volcanic rocks containing multi domain magnetic grains implications for the thellier paleointensity determination
topic Rock-magnetism
low-temperature demagnetization
domain structure
url http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2001/04/morales.pdf
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