Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Z. Bus"'
Autor:
D. Orešković, A. Madero Pohlen, I. Cvitković, J.F. Alen, M. Raguž, A. Álvarez-Sala de la Cuadra, G.J. Bazarra Castro, Z. Bušić, I. Konstantinović, V. Ledenko, C. Martínez Macho, D. Müller, M. Žarak, N. Jovanov-Milosevic, D. Chudy, T. Marinović
Publikováno v:
BMC Cancer, Vol 24, Iss 1, Pp 1-10 (2024)
Abstract Meningiomas are among the most common primary tumors of the central nervous system. Previous research into the meningioma histological appearance, genetic markers, transcriptome and epigenetic landscape has revealed that benign meningiomas s
Externí odkaz:
https://doaj.org/article/a19318282e6641b8830ac1c1f3b20d37
Akademický článek
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Publikováno v:
Tectonophysics. 474:343-352
The seismicity and the associated seismic hazard in the central part of the Pannonian region is moderate, however the vulnerability is high, as three capital cities are located near the most active seismic zones. In our analysis two seismically activ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::48552af308777dc4dc67f5e804534ad0
https://doi.org/10.1016/j.tecto.2009.02.045
https://doi.org/10.1016/j.tecto.2009.02.045
Autor:
Z. Bus, Zsolt Varga, Katalin Gribovszki, Szabolcs Leél-Őssy, Gergely Surányi, Győző Szeidovitz
Publikováno v:
Journal of Seismology. 12:21-33
The examination of speleothems in the Hajnoczy and Baradla caves (northeastern Hungary) allows estimating an upper limit for horizontal peak ground acceleration generated by paleoearthquakes. The density, the Young’s modulus and the tensile failure
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2244c10a6d847f0b04bacfe6c44c4d08
https://doi.org/10.1007/s10950-007-9068-9
https://doi.org/10.1007/s10950-007-9068-9
Publikováno v:
Acta Geodaetica et Geophysica Hungarica. 40:349-360
In this paper, research activities at the Theoretical Division of the Seismology Department of GGRI (in short: Seismological Observatory) are summarized. The reported investigations have been carried out since 1999, when the division was founded with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dbde61c6436eb128d3d8062f66a1d88
https://doi.org/10.1556/ageod.40.2005.3-4.7
https://doi.org/10.1556/ageod.40.2005.3-4.7
Publikováno v:
Acta Geodaetica et Geophysica Hungarica. 39:447-470
Analysing the areal distribution of earthquakes produced in the Carpathian Basin the conclusion can be drawn that only certain parts can be considered active along fracture lines, namely those parts which separate individually moving blocks. Generall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b46b8a28aaa3853f52d78cdd7ab74db7
https://doi.org/10.1556/ageod.39.2004.4.13
https://doi.org/10.1556/ageod.39.2004.4.13
Publikováno v:
Acta Geodaetica et Geophysica Hungarica. 39:327-337
The spatio-temporal patterns of the seismicity are shown. The earthquake occurrence is connected to the strain rate on the basis of Kostrov (1974) equation. It is shown that in the Pannonian Basin the seismic rates are 10-7-10-6. This values were der
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1203768482ed5e10c7256691bf153294
https://doi.org/10.1556/ageod.39.2004.2-3.14
https://doi.org/10.1556/ageod.39.2004.2-3.14
Autor:
Z. Bus
Publikováno v:
Acta Geodaetica et Geophysica Hungarica. 38:93-102
The crustal and uppermost mantle structure beneath the Matra Mountains has been investigated by means of the inversion of teleseismic P-wave receiver functions. Earthquakes recorded at the PSZ station in the period 1995-2000 with epicentral distances
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da397bf308eab9f2d622c14e5a33a24c
https://doi.org/10.1556/ageod.38.2003.1.11
https://doi.org/10.1556/ageod.38.2003.1.11
Publikováno v:
Acta Geodaetica et Geophysica Hungarica. 36:417-438
In this paper, a theory describing the possible origin of shallow depth earthquakes occurring within the sedimentary depressions of the Pannonian Basin is presented. In addition, the seismicity of Budapest is re-evaluated by synthetic seismogram base
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::26f5a78dce4cf59d4915ed8ef0d74188
https://doi.org/10.1556/ageod.36.2001.4.4
https://doi.org/10.1556/ageod.36.2001.4.4
Autor:
Z. Bus
Publikováno v:
Acta Geodaetica et Geophysica Hungarica. 36:189-205
Tomographic P-wave velocity inversion has been performed for the Pannonian region using first arrival times of local and regional events from the bulletins of the International Seismological Center and the Hungarian Earthquake Bulletins. The input da
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3eaff1a2433c66a756000679d8ca3c47
https://doi.org/10.1556/ageod.36.2001.2.6
https://doi.org/10.1556/ageod.36.2001.2.6