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

dc.contributor.author	Voss, J.
dc.contributor.author	Weinrebe, W.
dc.contributor.author	Schildknecht, F.
dc.contributor.author	Meissner, R.
dc.coverage.spatial	Moon
dc.date.accessioned	2020-07-10T21:11:09Z
dc.date.available	2020-07-10T21:11:09Z
dc.date.issued	1976
dc.identifier.citation	Proc. Lunar Sci. Conf. 7th (1976), p. 3133-3142.	en
dc.identifier.uri	https://hdl.handle.net/20.500.11753/1629
dc.description.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.	en
dc.format.extent	Page 3133-3142
dc.format.mimetype	application/pdf
dc.language.iso	en	en
dc.publisher	Pergamon Press	en
dc.relation.ispartofseries	LSI contribution ; no. 256
dc.subject	Seismic waves--Scattering	en
dc.subject	Moon	en
dc.title	Filter processes applied to the scattering parts of lunar seismograms for identifying the 300 km discontinuity and the lunar grid system	en
dc.type	Book chapter	en

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