Abstract
Deep-seated features of the Earth’s crust can be identified and characterized by the velocities or by the reflectivity of the transmitted seismic waves generated from artificial sources near the surface and recorded by seismographs distributed along profiles or fans.
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© 2001 Springer Science+Business Media Dordrecht
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Nicolich, R. (2001). Deep seismic transects. In: Vai, G.B., Martini, I.P. (eds) Anatomy of an Orogen: the Apennines and Adjacent Mediterranean Basins. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-9829-3_5
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DOI: https://doi.org/10.1007/978-94-015-9829-3_5
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-4020-6
Online ISBN: 978-94-015-9829-3
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