Observations of sPn from Swabian Alb earthquakes at the GRF array
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Published:
Dec 22, 1978
Keywords:
Swabian Alb earthquakes,
Observations of sPn,
Theoretical seismograms
Volumes
Vols. 1-18 (1924-1944), ISSN 0044-2801
Main Article Content
Abstract
A number of the largest earthquakes from the Swabian Alb recorded at the Grafenberg array have been examined (the geographic coordinates of the main station GRF are 49.69°N and 11.22°E; see Harjes and Seidl (1978) for a description of the array). It has been shown that the GRF records of some of the largest Swabian Alb earthquakes have a clear additional arrival between Pn and Pg.
ARK: https://n2t.net/ark:/88439/y003616
Permalink: https://geophysicsjournal.com/article/190
Article Details
How to Cite
Kind, R. (1978). Observations of sPn from Swabian Alb earthquakes at the GRF array. Journal of Geophysics, 45(1), 337-340. Retrieved from https://journal.geophysicsjournal.com/JofG/article/view/190
Section
References
Aichele, H. (1976) Interpretation refraktionsseismischer Messungen im Gebiet des Frankisch-Schwabischen Jura. Dissertation, University of Stuttgart
Harjes, H.-P., Seidl, D. (1978) Digital recording and analysis of broad-band seismic data at the Grafenberg (GRF)-array. J. Geophys. 44, 511-523
Kind, R. (1978) The reflectivity method for a hurried source. J. Geophys. 44, 603-612
Kind, R. (1979) Extensions of the reflectivity method. J. Geophys. 45 (In press)
Harjes, H.-P., Seidl, D. (1978) Digital recording and analysis of broad-band seismic data at the Grafenberg (GRF)-array. J. Geophys. 44, 511-523
Kind, R. (1978) The reflectivity method for a hurried source. J. Geophys. 44, 603-612
Kind, R. (1979) Extensions of the reflectivity method. J. Geophys. 45 (In press)