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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Format: | Article |
Language: | English |
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Universidad Nacional Autónoma de México, Instituto de Geofísica
2001-08-01
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Series: | Geofísica Internacional |
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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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format | Article |
id | doaj.art-9251960b26cb4047a597112ef40be8ab |
institution | Directory Open Access Journal |
issn | 0016-7169 |
language | English |
last_indexed | 2024-03-12T10:26:56Z |
publishDate | 2001-08-01 |
publisher | Universidad Nacional Autónoma de México, Instituto de Geofísica |
record_format | Article |
series | Geofísica Internacional |
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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