1887

Abstract

In deep reflection seismics, the acquistion parameters are optimized to image the middle and lower crust. Nevertheless, the knowledge about the velocity-depth structure of the sedimentary overburden is important for crustal studies. Macro-velocity models are needed, for example, for depth conversion of time horizons, for the application of depth migration algorithms and for tectonic balancing.

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/content/papers/10.3997/2214-4609.201408369
1998-06-08
2020-09-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408369
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