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Anica Otilia Placinta, Felix Borleanu, Emilia Popescu, Mircea Radulian and Ioan Munteanu
Romanian seismicity is mainly confined to the Eastern Carpathians Arc bend (ECAB), where strong subcrustal earthquakes (magnitude up to 7.9) are generated in a narrow lithospheric body descending into the mantle. The seismic activity in the overlying cru...
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