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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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Ramses Mourhatch and Swaminathan Krishnan
Seismic wave-propagation simulations are limited in their frequency content by two main factors: (1) the resolution of the seismic wave-speed structure of the region in which the seismic waves are propagated through; and (2) the extent of our understandi...
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Ramses Mourhatch and Swaminathan Krishnan
Kinematic source inversions of past earthquakes in the magnitude range of 6?8 are used to simulate 60 scenario earthquakes on the San Andreas fault. The unilateral rupture scenario earthquakes are hypothetically located at 6 locations spread out uniforml...
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Benjamin Edwards, Nadine Staudenmaier, Carlo Cauzzi and Stefan Wiemer
A method is described for the prediction of site-specific surface ground motion due to induced earthquakes occurring in predictable and well-defined source zones. The method is based on empirical Green?s functions (EGFs), determined using micro-earthquak...
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