Constructive interference—geophysical mythology re-examined

Iterative modification produces a best fit model that refines the definition of the subsurface geometry o1' major structures. We conclude that most reflections from the upper 20 km can be ascribed to the presence of sedimentary cover rocks (especially carbonates) and ophiolites juxtaposed against crystalline basement nappes. Thus, in this area, reflections appear to be principally due to lb'st-order lithologic contrasts. This study also demonstrates not only the importance of threedimensional effects (sideswipe) in interpreting seismic data, but also that these effects can be considered quantitatively through three-dimensional modeling.

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Constructive interference—geophysical mythology re-examined

Cited by 4 publications

References 3 publications

The bright Moho reflection in the 1986 Nevada PASSCAL seismic experiment

The bright Moho reflection in the 1986 Nevada PASSCAL seismic experiment

Seismic results at Kola and KTB deep scientific boreholes: velocities, reflections, fluids, and crustal composition

Crustal structure and reflectivity of the Swiss Alps from three‐dimensional seismic modeling: 2. Penninic Nappes

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