Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4694765 | Tectonophysics | 2007 | 18 Pages |
Abstract
Exposed rocks in the Ivrea and Serie dei Laghi zones show that amphibolites are interlayered with metapelites on a scale from 1 to 100 m. Because of the very large acoustic impedance contrast (20.34 ± 1.75 for amphibolites, 17.16 ± 0.4 for metapelites), they represent a very reflective portion in the middle-lower crust.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
V. Barberini, L. Burlini, A. Zappone,