Surface wave dispersion and upper mantle structure beneath southern Germany from joint inversion of network recorded teleseismic events

S Stange, W Friederich - Geophysical research letters, 1993 - Wiley Online Library
We have determined the dispersion of fundamental mode Rayleigh waves in Southern
Germany in the frequency range 4–50 mHz by simultaneously inverting data from 66 …

Surface wave dispersion and upper mantle structure beneath southern Germany from joint inversion of network recorded teleseismic events

S Stange, W Friederich - 1993 - arch.neicon.ru
We have determined the dispersion of fundamental mode Rayleigh waves in Southern
Germany in the frequency range 4–50 mHz by simultaneously inverting data from 66 …

Surface wave dispersion and upper mantle structure beneath southern Germany from joint inversion of network recorded teleseismic events

S Stange, W Friederich - Geophysical Research Letters, 1993 - ui.adsabs.harvard.edu
We have determined the dispersion of fundamental mode Rayleigh waves in Southern
Germany in the frequency range 4-50 mHz by simultaneously inverting data from 66 …

[引用][C] SURFACE WAVE DISPERSION AND UPPER MANTLE STRUCTURE BENEATH SOUTHERN GERMANY FROM JOINT INVERSION OF NETWORK …

S STANGE, W FRIEDERICH - Geophysical …, 1993 - American Geophysical Union