Úvod
Listování
Vyhledávání
Poslední vyhledávání
Šuplík
Připomínky a dotazy
Nápověda
Podrobnosti záznamu
Jméno
Janský, Jaromír
Autor článku
Comprehensive geophysical research of the seismogenic western part of the Bohemian Massif
Computation of ray amplitudes in radially inhomogeneous media with sloping Earth surface
Determining a 1-D velocity model of the uppermost crust from P and S arrival times using the neighbourhood algorithm: synthetic test
Discussion of the features of synthetic amplitude - distance curves of teleseismic P waves for global Earth models
Efficiency of individual CRL stations in seismic monitoring of the western Gulf of Corinth
Grid search hypocentral location method in simple 1-D media
Homogeneous velocity models of the West Bohemian swarm region obtained by grid search
Influence of some WEBNET stations on location of earthquakes in West Bohemian subregions Nový Kostel and Lazy
A layered model of the upper crust in the Aigion region of Greece, inferred from arrival times of the 2001 earthquake sequence
Layered velocity models of the Western Bohemia region
One-dimensional qP-wave velocity model of the upper crust for the West Bohemia/Vogtland earthquake swarm region
Reinterpretation of the travel times of P waves generated by quarry blasts in Western Bohemia
Relocation of earthquakes in West Bohemian/Vogtland subregions Lazy, Klingenthal and Plesná using the Master event method
Relocation of the 2001 earthquake sequence in Aegion, Greece
Seismic measurements along short profiles in western Bohemia during the Celebration 2000 experiment
Seismic regime of the West-Bohemian earthquake swarms region
Seizmický režim západočeské oblasti zemětřesných rojů
Shallow earthquakes: Shallower than expected?
Some aspects of the application of the Wiechert-Herglotz method to refraction data from Western Bohemia
Station correction of PATNET network for improvement of earthquake location in central part of Gulf of Corinth
Vertically inhomogeneous models of the upper crustal structure in the West-Bohemian seismoactive region inferred from the CELEBRATION 2000 refraction data