1887

Abstract

Deep electromagnetic sounding is an important part in a complex of methods, used in earthquakes prediction, as it permits to receive the information about changes of rocks resistivity p at rather large depth, where influence of seasonal factors does not appear, and it is possible to expect more noticeable variations of p because of approach to area of a formed seismic center.

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/content/papers/10.3997/2214-4609.201408393
1998-06-08
2021-06-15
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408393
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