Deep Electromagnetic Sounding of the Moon With Lunokhod 2 Data

L L Van'yan; I V Yegorov; E B Faynberg

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NASA NTRS · 19780005011

Deep Electromagnetic Sounding of the Moon With Lunokhod 2 Data

L L Van'yan·I V Yegorov·E B Faynberg

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Abstract

Results of electromagnetic sounding distinguished an outer high resistance shell about 200 km thick in the moon's structure. A preliminary petrological interpretation of the moon's layers indicated their origin as a consequence of differentiation of the initial peridotite material. Upon melting, 20% to 40% of the material melts and is removed to form a high resistance basaltic shell underlain by a layer of spinal peridotites enriched in divalent iron oxides and having a reduced resistance.

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L L Van'yan, I V Yegorov, E B Faynberg. 1977-01-01. Deep Electromagnetic Sounding of the Moon With Lunokhod 2 Data. https://ntrs.nasa.gov/citations/19780005011

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