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Filter processes applied to the scattering parts of lunar seismograms for identifying the 300 km discontinuity and the lunar grid system

Filter processes applied to the scattering parts of lunar seismograms for identifying the 300 km discontinuity and the lunar grid system

Voss, J.; Weinrebe, W.; Schildknecht, F.; Meissner, R.
URI: https://hdl.handle.net/20.500.11753/1629
Date: 1976

Abstract:

In spite of the large scattering of lunar seismic waves, an indication of a P-wave reflection from a discontinuity at a depth of about 300 km is obtained by means of polarization filtering of seismic data from recordings of artificial impacts.

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