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Cummings, Dominic Gerard
Seismic wave reflections recorded at the Earth’s surface provide a rich source of information about the structure of the subsurface. These reflections occur due to changes in the material properties of the Earth; in the acoustic approximation, thes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______463::2faab59ebe8fb00cd41637f32ceb28f9
https://hdl.handle.net/1842/40676
https://hdl.handle.net/1842/40676
