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Can the lunar crust be magnetized by shock: Experimental groundtruth

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  • Additional Information
    • Contributors:
      Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE); Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE); Institut Pprime UPR 3346 (PPrime Poitiers ); Université de Poitiers = University of Poitiers (UP)-École Nationale Supérieure de Mécanique et d’Aérotechnique Poitiers (ISAE-ENSMA)-Centre National de la Recherche Scientifique (CNRS); University of Arizona; University of Hawai'i Honolulu (UH); Ural Federal University Ekaterinburg (UrFU); Faculty of Physics MSU, Moscow; Lomonosov Moscow State University = Université d'État Lomonossov de Moscou Moscou (MSU); Kazan Federal University (KFU); Laboratoire Procédés et Ingénierie en Mécanique et Matériaux (PIMM); Conservatoire National des Arts et Métiers CNAM (CNAM)-Centre National de la Recherche Scientifique (CNRS)-Arts et Métiers Sciences et Technologies; HESAM Université - Communauté d'universités et d'établissements Hautes écoles Sorbonne Arts et métiers université (HESAM)-HESAM Université - Communauté d'universités et d'établissements Hautes écoles Sorbonne Arts et métiers université (HESAM)
    • Publication Information:
      HAL CCSD
      Elsevier
    • Publication Date:
      2010
    • Collection:
      Aix-Marseille Université: HAL
    • Abstract:
      International audience ; Since the first evidence of magnetized lunar crust, two mechanisms of magnetization have been suggested to account for lunar magnetism: thermoremanent magnetization (TRM), or shock remanent magnetization (SRM). We present here the first experimental acquisition of shock remanence by lunar rocks in the 0.1-2. GPa range, and discuss their implications for the interpretation of the paleomagnetic record of these rocks, as well as for the distribution of magnetic anomalies revealed by orbital data. Laser shock experiments in controlled magnetic fields performed on lunar mare basalts demonstrated that in the presence of an ambient field these rocks can be magnetized significantly starting at low pressure (~ 0.1. GPa). Hydrostatic loading experiments up to 1.8. GPa in controlled magnetic fields were used to impart piezo-remanent magnetization (an analogue for shock remanent magnetization) to mare basalts and highland regolith breccias. These experiments allow quantifying the shock remanence as a function of pressure and ambient field. Regarding the lunar antipodal magnetic anomaly model, our results show that lunar soils, regolith breccia and about 40% of lunar highland rocks (comprising regolith and impact-melt breccia) in the upper crust can be magnetized by low pressure shocks (< 10. GPa) to sufficient levels to account for the observed lunar antipodal anomalies. Therefore, the antipodal magnetization model appears to be plausible based on our experimental results, provided that several km of regolith and/or impact-processed rocks can be found at the antipodes of large impact basins. For typical lunar rocks dominated by multidomain FeNi with low Ni content, the maximum remanent magnetization that can be acquired during a low pressure shock (< 10. GPa) is about a third of what is expected for a TRM acquired in the same ambient field. Some mare basalts have identical coercivity spectra for their natural remanent magnetization and their SRM, leaving open the possibility that the NRM was ...
    • Accession Number:
      10.1016/j.epsl.2010.08.011
    • Online Access:
      https://hal.science/hal-02458332
      https://hal.science/hal-02458332v1/document
      https://hal.science/hal-02458332v1/file/PIMM_%20EPSL_2010_BERTHE.pdf
      https://doi.org/10.1016/j.epsl.2010.08.011
    • Rights:
      info:eu-repo/semantics/OpenAccess
    • Accession Number:
      edsbas.4E8F7DB