排序方式： 共有18条查询结果，搜索用时 359 毫秒
1.
Libuše Ruprechtová Klára Mrázová Jaroslav Fiedler Reviewer A. Zátopek 《Studia Geophysica et Geodaetica》1984,28(3):286-293
Summary The calculation procedures for determining epicentre parameters of weak near shocks with foci in Poland are discussed and tested for explosions with known epicentres.
m m¶rt; ¶rt; n¶rt;u num a uu m num nmua n auauu, u mu a mumuu u, n muu ¶rt;au uu mau. au mam nam (a. 4) nu nuuu na 71 u m ¶rt;u n¶rt; ¶rt; a auu ¶rt;a [11].相似文献
2.
Libuše Ruprechtová 《Studia Geophysica et Geodaetica》1958,2(4):397-399
Резюме Нзменение амплитуд объемных волн с расстоянием было изучено на основании б аемлетрясений, регистрированных 30 сейсмическими
станциями в эпицентральных расстояниях<30°. Из рисунков видно, что амплитуды продолных и поперечных волн меняются в изучаемых
расстояниях подобным образом, но минимум и максимум кривой (A
*, Δ) для волнSH подвинуты к ббльшим эпицентральным расстояниям чем в случае воумPH.
Address: Boční II, Praha 13-Spořilov. 相似文献
Address: Boční II, Praha 13-Spořilov. 相似文献
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Summary The core waves recorded at four seismograph stations in Central Europe were investigated with the aim to find the most suitable set of travel-time curves and a fitting model of the core structure. Another travel-time curve was constructed by means of time differences between the core phases. The differences in the features of the travel-time curves were studied using records of shallow, intermediate and deep shocks from the same focal region (Tonga). 相似文献
4.
Růžek Bohuslav Zedník Jan Klíma Karel Ruprechtová Libuše 《Studia Geophysica et Geodaetica》2000,44(2):175-187
The routine location of regional seismic events using data from the Czech National Seismological Network (CNSN) is based on Pn, Pg, Sn, Sg phases. A simple velocity model derived from Kárník's (1953) interpretation of an earthquake in Northern Hungary in 1951 has hitherto been used. At present, numerous local seismic networks record and locate local events, which are occasionally recorded at regional distances as well. Due to the relatively small dimensions of local networks, hypocenters (and origin times) determined by a local network might be considered as nearly exact from the point of view of regional-scale CNSN. The comparison of common locations performed by CNSN and by a local network enables us to estimate the accuracy of CNSN locations, as well as to optimize a simple velocity model. The joint interpretation of the CNSN bulletin and the catalogues of four local seismic networks WEBNET, OSTRAVA, KLADNO and LUBIN produced a new ID velocity model. The most frequent epicentral error in this model is less than 5 km, and most foci lie up to 15 km from the true position. The performed analysis indicates bimodal distribution of Sn residuals. 相似文献
5.
Jaromír Janský Libuše Ruprechtová Bernd Tittel Reviewer K. Pěč 《Studia Geophysica et Geodaetica》1977,21(3-4):267-273
Summary PKP-amplitudes of about 400 earthquakes from the SW Pacific Ocean observed at three stations in Central Europe were used to obtain the calibration function qPKP(D, h) based on the NEIS mb magnitudes. The calibration function allows us to determine the magnitudes for week earthquakes from the Pacific, for which the magnitudes from the P-waves cannot be derived. 相似文献
6.
Jaroslava Plomerová Libuše Ruprechtová Vladislav Babuška Reviewer A. Zátopek 《Studia Geophysica et Geodaetica》1979,23(3):288-295
17 mmu u uma uu 1976. anua 5 ¶rt;numu mauumu u¶rt;a mu u m na Pn, Pg, Sn u Sg. u¶rt; numm muam u mum ma¶rt;am¶rt;a ¶rt; uu mmu n¶rt;naam nu m m uamm aumm. ¶rt;am nu m mmu maua. 相似文献
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Dana Procházková Libuše Ruprechtová Zdeňka Schenková Arnošt Dudek Reviewer J. Janský 《Studia Geophysica et Geodaetica》1977,21(3-4):293-295
Summary The method of treatment of the macroseismic data obtained on the territory of the CSSR after the main 1976 Friuli earthquake is described and the preliminary results are confronted with the geologic structure. 相似文献
9.
Jaroslava Plomerová Libuše Ruprechtová Rewiever A. Zátopek 《Studia Geophysica et Geodaetica》1979,23(1):74-89
Summary The records of the first series of the North-Italian aftershock series from the period May–August 1976 at the stations Prhonice and Kaperské Hory were analyzed from the point of view of the verification of the travel-time tables used for the interpretation of near earthquake seismograms and of the determination of the short-period body wave magnitudes for near shocks. Also the time-energy distribution was investigated for a 90 days period. 相似文献
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