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- W9942114 abstract "Weak and strong intermediate-depth Vrancea earthquakes occur in a small zone beneath the southeastern Carpathian Mountains. Despite their small seismogenic dimension, the seismic moment release is unusually high. During the last century, four major earthquakes occurred in this source zone which is confined to an area of only 20 x 60 km2. The focal depths range from 60 to 170 km, but a few events were found in depths to about 220 km. In this paper we analyze the October 27, 2004 Mw = 5.8 event and the aftershock pattern in the context of the background seismicity. We further present ground motion maps for the mainshock using the recordings of the accelerometer networks installed in Romania and the macroseismic intensities as observed by the Internet community provided by the United States Geological Survey. The combination of these instrument and Internet-based observations enabled the construction of ground motion maps covering the whole territory of Romania and its bordering countries. The geographical pattern of the peak ground acceleration as well as the seismic intensity of the moderate October 2004 earthquake show the well-known northeast-southwest trending of the maximum values as displayed by the big events of 1940, 1977, 1986 and 1990. The growing community of Internet users will provide denser, extensive and even cross-border information on the effects of future strong Vrancea earthquakes than instrument observations alone can do." @default.
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- W9942114 date "2009-12-02" @default.
- W9942114 modified "2023-09-26" @default.
- W9942114 title "Ground Motion Patterns Of Intermediate-Depth Vrancea Earthquakes: The October 27, 2004 Event" @default.
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- W9942114 doi "https://doi.org/10.1007/978-1-4020-9242-8_3" @default.
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