1887

Abstract

The generation and recording of very low seismic frequencies in surface and borehole seismic enable geophysical applications such as inversion to acoustic impedance and deep imaging beneath high velocity and absorbing formations. A field experiment was d

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/content/papers/10.3997/2214-4609.201400273
2009-06-08
2021-11-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400273
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