By Bruce A. Bolt (auth.), F. Wenzel, D. Lungu, O. Novak (eds.)
This quantity comprises the main proper peer-reviewed papers provided on the First foreign Workshop on Vrancea Earthquakes, held in Bucharest on November 1-4, 1997. powerful earthquakes within the Romanian Vrancea zone have prompted a excessive toll of casualties and large harm during the last a number of centuries. With a second value of 7.4, the 1977 earthquake prompted greater than 1500 casualties, the vast majority of them in Bucharest. The contributions tackle key difficulties of seismotectonics of the Vrancea quarter and similar robust floor movement, chance overview, website results and microzonation, structural harm and earthquake resistant layout, chance evaluate and catastrophe administration from a world and nearby point of view. This record of themes indicates the varied contributions from the multidisciplinary fields of geosciences, geophysics, seismology, geology, civil engineering, urban making plans, and emergency reduction practices. This e-book is of worth for scientists drawn to earthquake possibility and seismic chance examine in addition to for seismologists, geophysicists and Earth scientists. it's also invaluable for experts liable for public protection and common chance mitigation plans and for coverage companies.
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Extra info for Vrancea Earthquakes: Tectonics, Hazard and Risk Mitigation: Contributions from the First International Workshop on Vrancea Earthquakes, Bucharest, Romania, November 1–4, 1997
Example text
P. and Apopei, I. , March 1991. N. (1970) Tectonic stress and the spectra of seismic shear waves, J. Ceophys. Res. 75,4997-5009. Chin, Byau-Heng and Aki, K. (1991) Simultaneous determination of source, path and recording site effects on strong ground motion during the Lorna Prieta earthquake - a preliminary result on pervasive nonlinear site effect, Bull. Seism. Soc. Am. 81, 1859-1884. Constantinescu, L. and Enescu, D. (1964) Fault-plane solutions for some Roumanian earthquakes and their seismotectonic implications, 1.
Characteristics of Vrancea Seismicity The seismicity of the Vrancea region in the SE Carpathians is characterized by the occurrence of intermediate depth earthquakes in an amazingly narrow epicentral and hypocentral region. The epicentral area is confined to about 30 x 70 km (Fig. 1). Earthquakes occur between 70 and 200 km depth within an almost vertical column. Deeper and shallower events have been recorded but only with small magnitudes. Depth and estimated moment magnitude (Mw ) of all instrumentally recorded events are summarized in Oncescu and Bonjer (1997).
9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20. 21. 22. 23. 24. 25. 26. 27. 25 Koch, M. (1985) Nonlinear inversion of local seismic travel times for the simultaneous determination of the 3D-velocity structure and hypocentres - application to the seismic zone Vrancea, J. Geophys. 56,160-173. Kostrov, V (1974), Seismic moment and energy of earthquakes, and seismic flow of rocks, Izv. Acad. Sci. USSR, Phys. Solid EaTth 1, 23-44. , and Popa, M. (1997) Teleseismic travel-time tomography of the compressional-wave velocity structure in the Vrancea zone, Romania, Abstract, AGU Fall Meeting, San Francisco, USA.