1887

Abstract

3 seismic source types, vibrators, explosives and weight drop are compared. A seismic<br>wavelet is estimated for each source. The wavelets are normalized using specific source<br>parameters: mass for the explosives, mass and heights for the weight drop, Peak force and<br>sweep rate for the vibrators. The observed amplitude levels are compared to the input energy.

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/content/papers/10.3997/2214-4609.20147513
2008-10-13
2020-02-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20147513
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