Temperature and structure of the moon according to electrical conductivity data on its interior

Details Temperature and structure of the moon according to electrical conductivity data on its interior Temperature and structure of the moon according to electrical conductivity data on its interior

Jan 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975stin...7515565o&link_type=abstract

"Temperature and structure of the moon according to electrical conductivity data on its interior NASA Transl. into ENGLISH of "K

Mathematics

Logic

Electrical Resistivity, Lunar Temperature, Lunar Topography, Lunar Composition, Lunar Rocks, Lunar Surface

Scientific paper

Based on the familiar temperature dependence of conductivity, which relates electrical conductivity to parameters characterizing the petrological composition of rocks, a temperature estimate of the lunar interior was obtained: the temperature within the moon rises sharply from 250 K in the near-surface layer to 800 K at 200 km from the surface and then, beginning from 400 km, tends to its adiabatic value, reaching 1050 K at 600 km. Three major regions of the lunar interiors can be distinguished: 0-200 km, 200-600 km, and the region lying below 600 km (pyroxenitic, peridotitic, and olivinic shells, respectively).

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