A technique of deep electromagnetic sounding of the moon using simultaneous magnetic-field measurements at two lunar surface sites is described. The method, used with the assumption that deep electrical conductivity is a function only of lunar radius, has the advantage of allowing calculation of the external driving field from two surface-site measurements only and therefore does not require data from a lunar orbiting satellite. A transient-response calculation is presented for the example of a magnetic-field discontinuity, measured simultaneously by Apollo 16 and Lunokhod 2 surface magnetometers.


    Zugriff

    Zugriff über TIB

    Verfügbarkeit in meiner Bibliothek prüfen


    Exportieren, teilen und zitieren



    Titel :

    Electromagnetic sounding of the moon using Apollo 16 and Lunokhod 2 surface magnetometer observations /preliminary results/


    Beteiligte:
    Vanian, L. L. (Autor:in) / Vnutchokova, T. A. (Autor:in) / Fainberg, E. B. (Autor:in) / Eroschenko, E. A. (Autor:in) / Dyal, P. (Autor:in) / Parkin, C. W. (Autor:in) / Daily, W. D. (Autor:in)

    Erschienen in:

    Erscheinungsdatum :

    01.11.1977


    Medientyp :

    Sonstige


    Format :

    Keine Angabe


    Sprache :

    Englisch