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The low-temperature magnetic signature of Fe-rich serpentine in CM2 chondrites: Comparison with terrestrial cronstedtite and evolution with the degree of alteration

Agnès Elmaleh 1 Serena Chiara Tarantino 2 Michele Zema 2 Bertrand Devouard 3 Michel Fialin 4 
1 IMPMC - Institut de minéralogie et de physique des milieux condensés
2 Dipartimento di Scienze della Terra e dell'Ambiente
3 LMV - Laboratoire Magmas et Volcans
4 Plateforme Camparis - Plateforme analytique MEN (Microanalyses en sciences de l’Environnement) [Paris]
ECCE TERRA - Observatoire des sciences de l'univers Ecce Terra [Paris]
Keywords : bulk magnetometry crystal-chemistry of serpentines spin glass behavior asteroidal processes hydrothermal alteration
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https://hal.archives-ouvertes.fr/hal-00720273
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Submitted on : Friday, March 18, 2022 - 3:40:27 PM
Last modification on : Thursday, June 9, 2022 - 10:12:02 AM
Long-term archiving on: : Sunday, June 19, 2022 - 7:10:00 PM

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Geochem Geophys Geosyst - 2012...
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UNIV-ST-ETIENNE | INSU | UNIV-PARIS7 | ENS-PARIS | UPMC | PRES_CLERMONT | CNRS | IMPMC | ALLINSP | LMV | ACL-SF | PSL | OPGC | SORBONNE-UNIVERSITE | SU-SCIENCES | UMS-3455 | UDL | UNIV-PARIS | SU-TI

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Agnès Elmaleh, Serena Chiara Tarantino, Michele Zema, Bertrand Devouard, Michel Fialin. The low-temperature magnetic signature of Fe-rich serpentine in CM2 chondrites: Comparison with terrestrial cronstedtite and evolution with the degree of alteration. Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2012, 13, pp.Q05Z42. ⟨10.1029/2011GC003964⟩. ⟨hal-00720273⟩

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