Overview and new data on the active tectonics of Bulgaria: towards a comprehensive seismotectonic map
Author(s)
Language
English
Obiettivo Specifico
2T. Deformazione crostale attiva
Status
Published
JCR Journal
N/A or not JCR
Peer review journal
Yes
Journal
Issue/vol(year)
1-2/25 (2013)
Pages (printed)
67-82
Date Issued
2013
Subjects
04. Solid Earth
Abstract
This paper presents a discussion on some aspects of the active tectonics in Bulgaria based on available literature data as well as recent
research mainly focused on the identification and characterization of active faults in selected key areas. In particular, through tectonic,
GPS and remote sensing data, also coupling geological observations with seismological data, we present here 1) a comprehensive
map of major active faults in Bulgaria, although still in progress, and 2) a detailed study of various active structures, in particular in
the Sofia Graben, Struma valley and surrounding regions.
Our research highlights the occurrence in south-west Bulgaria of several major active faults, the majority of which are normal faults
accommodating a roughly N-S to NNE-SSW extension, in line with GPS data and analysis of the instrumental seismicity. The extensional
stress field, with associated tectonic and seismic activity, is likely to be related to the northern extent of the Aegean extensional
system and its recent evolution. In the Balkan mountains area the tectonic activity is somehow more complex, responding to the
interplay of the northward propagation of the Aegean extension and the influence of a roughly E-W compression, which determines
local shear zones.
research mainly focused on the identification and characterization of active faults in selected key areas. In particular, through tectonic,
GPS and remote sensing data, also coupling geological observations with seismological data, we present here 1) a comprehensive
map of major active faults in Bulgaria, although still in progress, and 2) a detailed study of various active structures, in particular in
the Sofia Graben, Struma valley and surrounding regions.
Our research highlights the occurrence in south-west Bulgaria of several major active faults, the majority of which are normal faults
accommodating a roughly N-S to NNE-SSW extension, in line with GPS data and analysis of the instrumental seismicity. The extensional
stress field, with associated tectonic and seismic activity, is likely to be related to the northern extent of the Aegean extensional
system and its recent evolution. In the Balkan mountains area the tectonic activity is somehow more complex, responding to the
interplay of the northward propagation of the Aegean extension and the influence of a roughly E-W compression, which determines
local shear zones.
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tensor determination in the European Mediterranean area – initial
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Burchfiel B.C., Nakov R., Tzankov Tz. and Royden L. (2000). Cenozoic
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Aegean extensional regime. In: “Tectonics and Magnetism in Turkey
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J.D.A. (Eds.), «Geol. Soc. Spec. Publ.», 173, 325-352.
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of the Geophysical Institute», Bulgarian Academy of Sciences,
12, 79-105.
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the Alpine orogen in the Eastern Mediterranean and the Carpathian-
Balkan area. «Geotectonics, Tectonophysics and Geodynamics», 22,
45-70 (in Bulgarian with abstract in English).
Dabovski C., Boyanov I., Khrischev Kh., Nikolov T., Sapunov I, Yanev Y.
and Zagorchev I. (2002). Structure and Alpine evolution of Bulgaria.
«Geologica Balkanica», 32, 9-15.
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the evolution of the Alpine system. «Geol. Soc. Am. Bull.», 84, 3137-
3180.
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Acad. Sci., Geophys. Inst., Seismol. Dep., 39 pp.
Dineva S., Batllo J., Mihaylov D. and van Eck T. (2002). Source parameters
of four strong earthquakes in Bulgaria and Portugal at
the beginning of the 20th century. «J. Seismol.», 6, 1, 99-123.Dinter D. (1998). Late Cenozoic extension of the Alpine collisional
orogen in northeastern Greece, origin of the north Aegean basin.
«Geol. Soc. Am. Bull.», 110, 1208-1230.
Dobrev N. (1999a). Geological hazard processes in Simitli graben. PhD
Thesis, Geological Institute, Bulgarian Academy of Sciences, Sofia.
181 pp.
Dobrev N. (1999b). Fault pattern in the southern part of the Simitli
graben (SW Bulgaria). In: Proceedings of the 2nd Congress of Balkan
Geophysical Society, 5-9 July 1999, Istanbul, Turkey.
Dobrev N. (2011). 3D Monitoring of Active Fault Structures In The Krupnik-
Kresna Seismic Zone, Sw Bulgaria. «Acta Geodyn. Geomater.», 8,
4 (164), 377-388.
Dobrev N. and Kostak B. (2000). Monitoring tectonic movements in the
Simitli Graben, SW Bulgaria. «Eng. Geol.», 57, 179-192.
Dobrev N., Frangov G. and Drakatos G. (2004). Monitoring of active
faults along the Strouma Fault Zone, SW Bulgaria. In: Proceedings
of the 5th International Symposium on Eastern Mediterranean
Geology, Thessaloniki, Greece, 14-20 April 2004, II, 687-690.
Dobrev N. and Petrov P. (2007). Terrain Effects Caused by 1904 Krupnik
Earthquake. In: Proceedings of International Project “Seismo-Hydrogeological
Vulnerability of the Environment and Society in the
Balkan Region”, Second Meeting, 22-26 November 2006, Sofia, 139-
164.
Dziewonski A.M., Chou T.-A. and Woodhouse J.H. (1981). Determination
of earthquake source parameters from waveform data for
studies of global and regional seismicity, «J. Geophys. Res.», 86 (B4),
2825-2852.
Ekström G., Dziewonski A. M., Maternosvskaya N.N. and Nettles, M.
(2005). Global seismicity of 2003: Centroid-moment tensor solutions
for 1087 earthquakes. «Phys. Earth. Planet. In.», 148, 327-351.
Frohlich C. (1992). Triangle diagrams: ternary graphs to display similarity
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