1887

Abstract

The measurement of a man made signal S, masked by natural noises of mean strenght N, is common to many geophysical methods; but the Author will take into account only the case of the geoelectrical D.C. current surveys about which he reached a sufficient experience. The problem arose when deep sounding where carried out by means of Dipole-Dipole arrays and with long distances between the two dipoles,up to twenty kilometers.

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/content/papers/10.3997/2214-4609.201410767
1991-05-28
2020-08-05
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410767
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