Zobrazeno 1 - 10
of 26
pro vyhledávání: '"D. G. Panagiotopoulos"'
Autor:
C. B. Papazachos, Emilie E. E. Hooft, Nikolaos Theodulidis, Panagiotis Hatzidimitriou, Nikolaos Chatzis, D. R. Toomey, Michael Warner, Marios Anthymidis, George Vougioukalakis, Ben Heath, Joanna Morgan, Michelle Paulatto, D. G. Panagiotopoulos
We investigate the geometry of the metamorphic basement of the Santorini volcanic island using ambient noise data to determine the pre-Alpine/pre-volcanic bedrock structure. The geometry of pre-volcanic Santorini is important in order to constrain th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f6fcec8bcd7abe538578b7ec6932c1f
https://doi.org/10.5194/egusphere-egu21-7968
https://doi.org/10.5194/egusphere-egu21-7968
Autor:
Olaf Bubenzer, R. Altherr, D. G. Panagiotopoulos, Bernhard Eitel, Christoph Siart, H. P. Meyer, Ingmar Holzhauer, Gerd Schukraft, Stefan Hecht
Publikováno v:
Quaternary International. 216:75-92
Sediment-filled karst depressions (e.g. dolines) have rarely been used as geoarchives in Greece due to an uncertainty about the thickness of accumulations and their vague suitability for palaeoenvironmental research. However, such terrestrial proxy-d
Autor:
C. B. Papazachos, B. C. Papazachos, Emmanuel M. Scordilis, G. F. Karakaisis, D. G. Panagiotopoulos
Publikováno v:
Journal of Seismology. 14:273-288
Decelerating generation of preshocks in a narrow (seismogenic) region and accelerating generation of other preshocks in a broader (crit- ical) region, called decelerating-accelerating seis- mic strain (D-AS) model has been proposed as appropriate for
Autor:
E. Karagianni, Panagiotis Hatzidimitriou, C. B. Papazachos, I. Dimitriadis, M. Rische, Marco Bohnhoff, Thomas Meier, D. G. Panagiotopoulos
Publikováno v:
Tectonophysics
The volcanic center of Santorini Island is the most active volcano of the southern Aegean volcanic arc. Α dense seismic array consisting of fourteen portable broadband seismological stations has been deployed in order to monitor and study the seismo
Autor:
C. B. Papazachos, Alessandro Vuan, Giuliano F. Panza, E. Karagianni, Peter Suhadolc, D. G. Panagiotopoulos
Publikováno v:
Geophysical Journal International. 160:127-143
SUMMARY The purpose of this work is to derive a 3-D tomographic image of the shear wave velocity structure of the crust—uppermost mantle in the Aegean area using the group velocities of Rayleigh wave fundamental mode. The database consists of 185 r
Autor:
Alessandro Vuan, Anastasia Kiratzi, Peter Suhadolc, Giuliano F. Panza, C. B. Papazachos, D. G. Panagiotopoulos, E. Karagianni, Keith Priestley, Denis Hatzfeld, Konstantinos Makropoulos, B. C. Papazachos
Publikováno v:
Tectonophysics. 358:187-209
Data from a large-scale experiment which took place in Greece during the period January–July 1997 have been used to investigate the structure of the Aegean area using surface waves. During this experiment, 30 seismic broadband instruments were depl
Publikováno v:
Journal of Geodynamics. 26:297-307
The seismicity of western Macedonia is examined in the present paper. On the basis of historical information as well as on instrumental data it is found that this area is characterized by low seismicity. The focal region of the Grevena-Kozani 1995 ea
Publikováno v:
Pure and Applied Geophysics PAGEOPH. 149:173-217
Investigation of the time-dependent seismicity in 274 seismogenic regions of the entire continental fracture system indicates that strong shallow earthquakes in each region exhibit short as well as intermediate term time clustering (duration extendin
Publikováno v:
Journal of Geophysical Research: Solid Earth. 100:12405-12422
Compressional velocity structure of the crust and the upper mantle in southeastern Europe (broader Aegean area) is studied by inverting residuals of the first P arrivals from earthquakes in this region (16°E-31°E, 34°N-43°N). The data used are fr
Autor:
D. G. Panagiotopoulos
Publikováno v:
Natural Hazards. 11:17-43
Instrumental and historical information on strong main-shocks for 13 seismogenic sources along the seismic zone of the Solomon Islands and New Hebrides has been used to show that the interevent time,Tt (in years), between two strong earthquakes and t