Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteorite
Hysteresis properties of twenty individual chondrules from a ~50 cc piece of the Allende carbonaceous chondritic meteorite, with diameters between about 0.08 and 0.44 cm are reported. Coercive force Hc varies from about 3 mT to 32.5 mT. Magnetic remanence to saturation magnetization ratios Mr/Ms var...
Main Authors: | , |
---|---|
Format: | Article |
Language: | English |
Published: |
Universidad Nacional Autónoma de México, Instituto de Geofísica
2002-02-01
|
Series: | Geofísica Internacional |
Subjects: | |
Online Access: | http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2002/02/flores.pdf |
_version_ | 1797761409843462144 |
---|---|
author | Jaime Urrutia-Fucugauchi Daniel Flores-Gutiérrez |
author_facet | Jaime Urrutia-Fucugauchi Daniel Flores-Gutiérrez |
author_sort | Jaime Urrutia-Fucugauchi |
collection | DOAJ |
description | Hysteresis properties of twenty individual chondrules from a ~50 cc piece of the Allende carbonaceous chondritic meteorite, with diameters between about 0.08 and 0.44 cm are reported. Coercive force Hc varies from about 3 mT to 32.5 mT. Magnetic remanence to saturation magnetization ratios Mr/Ms vary from about 0.025 to 0.25. If magnetite is the main magnetic mineral, then this variation in hysteresis parameters suggests a range of particle grain sizes and shapes, corresponding to pseudo-single domain PSD and multidomain MD states. No chondrules with single domain SD states were observed. Simple relationships among mass, density, size and shape of chondrules and magnetic hysteresis properties are proposed. Three groups with characteristic coercitivity values are distinguished: (a) group 1 for chondrules with Hc between 0 and 5 mT; (b) group 2 for those with Hc between 5 and 15 mT; and (c) group 3 for those with Hc larger than 15 mT. Group 1 chondrules plot within the MD field, group 2 chondrules plot in the PSD and intermediate fields with low Mr/Ms values, and group 3 chondrules plot in the PSD field with high Mr/Ms values. |
first_indexed | 2024-03-12T19:12:36Z |
format | Article |
id | doaj.art-eae34fb19a7745d6be690171a45f1ce9 |
institution | Directory Open Access Journal |
issn | 0016-7169 |
language | English |
last_indexed | 2024-03-12T19:12:36Z |
publishDate | 2002-02-01 |
publisher | Universidad Nacional Autónoma de México, Instituto de Geofísica |
record_format | Article |
series | Geofísica Internacional |
spelling | doaj.art-eae34fb19a7745d6be690171a45f1ce92023-08-02T05:47:53ZengUniversidad Nacional Autónoma de México, Instituto de GeofísicaGeofísica Internacional0016-71692002-02-01412179188Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteoriteJaime Urrutia-FucugauchiDaniel Flores-GutiérrezHysteresis properties of twenty individual chondrules from a ~50 cc piece of the Allende carbonaceous chondritic meteorite, with diameters between about 0.08 and 0.44 cm are reported. Coercive force Hc varies from about 3 mT to 32.5 mT. Magnetic remanence to saturation magnetization ratios Mr/Ms vary from about 0.025 to 0.25. If magnetite is the main magnetic mineral, then this variation in hysteresis parameters suggests a range of particle grain sizes and shapes, corresponding to pseudo-single domain PSD and multidomain MD states. No chondrules with single domain SD states were observed. Simple relationships among mass, density, size and shape of chondrules and magnetic hysteresis properties are proposed. Three groups with characteristic coercitivity values are distinguished: (a) group 1 for chondrules with Hc between 0 and 5 mT; (b) group 2 for those with Hc between 5 and 15 mT; and (c) group 3 for those with Hc larger than 15 mT. Group 1 chondrules plot within the MD field, group 2 chondrules plot in the PSD and intermediate fields with low Mr/Ms values, and group 3 chondrules plot in the PSD field with high Mr/Ms values.http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2002/02/flores.pdfAllende meteoriterock-magnetismchondritic meteoriteschondrulesSolar Nebula |
spellingShingle | Jaime Urrutia-Fucugauchi Daniel Flores-Gutiérrez Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteorite Geofísica Internacional Allende meteorite rock-magnetism chondritic meteorites chondrules Solar Nebula |
title | Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteorite |
title_full | Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteorite |
title_fullStr | Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteorite |
title_full_unstemmed | Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteorite |
title_short | Hysteresis properties of chondritic meteorites: New results for chondrules from the Allende meteorite |
title_sort | hysteresis properties of chondritic meteorites new results for chondrules from the allende meteorite |
topic | Allende meteorite rock-magnetism chondritic meteorites chondrules Solar Nebula |
url | http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2002/02/flores.pdf |
work_keys_str_mv | AT jaimeurrutiafucugauchi hysteresispropertiesofchondriticmeteoritesnewresultsforchondrulesfromtheallendemeteorite AT danielfloresgutierrez hysteresispropertiesofchondriticmeteoritesnewresultsforchondrulesfromtheallendemeteorite |