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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... ver más
Revista: Geosciences    Formato: Electrónico

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