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VRANCEA99—the crustal structure beneath the southeastern Carpathians and the Moesian Platform from a seismic refraction profile in Romania
- F. Hauser, V. Rǎileanu, +4 authors A. Schulze
- Geology
- 30 October 2001
The VRANCEA99 seismic refraction experiment is part of an international and multidisciplinary project to study the intermediate depth earthquakes of the Eastern Carpathians in Romania. As part of the… Expand
Seismic crustal structure between the Transylvanian Basin and the Black Sea, Romania
- F. Hauser, V. Rǎileanu, +4 authors C. Prodehl
- Geology
- 5 February 2007
Abstract In order to study the lithospheric structure in Romania a 450 km long WNW–ESE trending seismic refraction project was carried out in August/September 2001. It runs from the Transylvanian… Expand
PHYSICAL AND DYNAMIC PROPERTIES OF THE SHALLOW SEDIMENTARY ROCKS IN THE BUCHAREST METROPOLITAN AREA
- A. Bălă, V. Rǎileanu, Ion Zihan, V. Ciugudean, B. Grecu
- Geology
- 2006
New seismic measurements are performed in the Bucharest area with the purpose of defining better the physical and dynamic properties of the shallow sedimentary rocks. Down-hole seismic measurements… Expand
- 23
- 5
- PDF
Crustal properties from S-wave and gravity data along a seismic refraction profile in Romania
- V. Rǎileanu, A. Bala, F. Hauser, C. Prodehl, W. Fielitz
- Geology
- 9 December 2005
VRANCEA'99 is a seismic refraction line that was carried out in 1999 to investigate the deep structure and physical properties of the upper lithosphere of the southeastern Carpathians and its… Expand
Crustal constraints on the origin of mantle seismicity in the Vrancea Zone, Romania: The case for active continental lithospheric delamination
- J. Knapp, C. Knapp, V. Rǎileanu, L. Maţenco, V. Mocanu, C. Dinu
- Geology
- 9 December 2005
Abstract The Vrancea zone of Romania constitutes one of the most active seismic zones in Europe, where intermediate-depth (70–200 km) earthquakes of magnitude in excess of M w = 7.0 occur with… Expand
Mantle earthquakes in the absence of subduction? Continental delamination in the Romanian Carpathians
- M. A. Fillerup, J. Knapp, C. Knapp, V. Rǎileanu
- Geology
- 1 October 2010
The Vrancea seismogenic zone of Romania is a steeply NW-dipping volume (30 × 70 × 200 km) of intermediate-depth seismicity in the upper mantle beneath the bend zone of the Eastern Carpathians. It is… Expand
CRUSTAL SEISMICITY AND ACTIVE FAULT SYSTEMS IN ROMANIA
- A. Bala, V. Rǎileanu, C. Dinu, M. Diaconescu
- 2015
The most significant seismicity in Romania is located in a relatively small area – the Vrancea seismogenic zone, where 2–3 intermediate depth strong earthquakes (Mw > 7.0) occur in a century.… Expand
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- 2
- PDF
Dynamic properties of the Quaternary sedimentary rocks and their influence on seismic site effects. Case study in Bucharest City, Romania
- A. Bălă, B. Grecu, V. Ciugudean, V. Rǎileanu
- Geology
- 2009
Bucharest is one of the cities most affected by earthquakes in Europe. Situated at 150–170 km distance from Vrancea epicentral zone, Bucharest had suffered many damages due to high energy Vrancea… Expand
CRUSTAL MODELS IN ROMANIA - I. MOESIAN PLATFORM
- V. Rǎileanu, D. Tǎtaru, B. Grecu
- Geology
- 2012
A set of crustal data collected in the last decades across the Moesian platform are processed in order to derive a crustal model. New crustal model comprises maps with depths to the top of lower… Expand
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- 1
- PDF
Characteristics of Romanian lithosphere from deep seismic reflection profiling
- V. Rǎileanu, C. Diaconescu, F. Radulescu
- Geology
- 15 December 1994
Abstract The tectonic units of Romania contain both Alpine orogenic regions and platforms. The investigations of crustal structure by near-vertical reflection seismic profiling are based on less than… Expand