Summary
The level of microseismic noise is studied at locations in the Western Carpathians where, apart from the vertical component of the noise, also its horizontal component was recorded by a broad-band seismograph. The amplitudes of the permanent noise in the horizontal component ranged from 10 to 83 nm and, at most locations, the predominant periods T>0.45 s, although the predominant periods of the vertical component in the Carpathian region are mostly within the interval T ≐ 0.24–0.37 s.
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References
K. Holub: Level of Seismic Noise in the West Carpathians. Travaux Inst. Géophys. Acad. Tchécosl. Sci. No 306, Geofysikální sborník 1969, Academia, Praha 1972.
K. Holub: The Level of Seismic Noise Along the International Deep Seismic Sounding Profiles VI and VII in the Bohemian Massif. Travaux Inst. Géophys. Tchécosl. Sci. No 437, Geofysikální sborník 1975, Academia, Praha (in press).
A. Zátopek: Šíření východoalpských zemětřesení Českým masivem. Publ. Inst. Géophys. Nat. Tchécosl., Tr. Spéc. No 3, Praha 1948.
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Holub, K. A note on the microseismic noise in the western carpathians. Stud Geophys Geod 20, 203–208 (1976). https://doi.org/10.1007/BF01626055
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DOI: https://doi.org/10.1007/BF01626055