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First International Conference on MOLDAVIAN RISKS – FROM ...

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<str<strong>on</strong>g>First</str<strong>on</strong>g> <str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> <str<strong>on</strong>g>C<strong>on</strong>ference</str<strong>on</strong>g> <strong>on</strong> <strong>MOLDAVIAN</strong> <strong>RISKS</strong> - <strong>FROM</strong> GLOBAL TO LOCAL SCALE<br />

16-19 May 2012, Bacau, Romania<br />

SEISMOGENIC ZONES AND SEISMIC HAZARD AT LOCAL<br />

AND REGIONAL SCALES IN MOLDAVIA<br />

Mircea Radulian, Neculai Mandrescu<br />

Nati<strong>on</strong>al Institute for Earth Physics, Magurele, Ilfov, Department of Seismology<br />

Corresp<strong>on</strong>ding author: Mircea Radulian, mircea@infp.ro<br />

Abstract: The paper is presenting an overall characterizati<strong>on</strong> of the seismotect<strong>on</strong>ics and<br />

seismicity in the Moldavia regi<strong>on</strong> as fundamentals to define the seismogenic z<strong>on</strong>es and the<br />

associated seismic hazard for this regi<strong>on</strong>. The hazard level is clearly c<strong>on</strong>trolled by the<br />

earthquake activity in the Vrancea regi<strong>on</strong>. Some effects recorded at the southern boundary<br />

of the Moldavian Platform (Galati <strong>–</strong> Braila) are induced by the shallow seismicity located<br />

al<strong>on</strong>g the system of NW-SE oriented faults (Peceneaga-Camena, Sfantu Gheorghe,<br />

Trotus), crossing the northern Dobrogea and terminating in the Barlad Depressi<strong>on</strong>. The<br />

distributi<strong>on</strong> of the seismic hazard due to the Vrancea earthquakes is analyzed in c<strong>on</strong>necti<strong>on</strong><br />

with the revised macroseismic data and instrumentally recorded accelerograms. The effects<br />

of the focal depth, source directivity and seismic wave attenuati<strong>on</strong> and their impact <strong>on</strong><br />

hazard level are investigated. The amplificati<strong>on</strong> of the ground moti<strong>on</strong> due to the shallow<br />

geological layers and res<strong>on</strong>ance frequency in the Bacau area and surroundings are<br />

estimated <strong>on</strong> the basis of borehole data. Implicati<strong>on</strong>s <strong>on</strong> management strategy to mitigate<br />

earthquake risk are finally discussed.<br />

Key words: seismogenic z<strong>on</strong>e, Vrancea earthquake, seismic hazard, microz<strong>on</strong>ati<strong>on</strong>, Moldavia,<br />

Bacau<br />

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