Earth Thermal Field Variations in Dependence from Lunisolar Tides (by Vorotilovo Deep Well Observations)

Details Earth Thermal Field Variations in Dependence from Lunisolar Tides (by Vorotilovo Deep Well Observations) Earth Thermal Field Variations in Dependence from Lunisolar Tides (by Vorotilovo Deep Well Observations)

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1037e&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1037

Physics

Scientific paper

The variations of upper crust geophysical parameters (temperature,
seismic-acoustic, etc) show the dependence from tidal gravity
variations. In accordance with our results, the main dissipation in
Earth's upper core takes place in the depth interval 1800 2000 meters.

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