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Deep Seismic Sounding of the Earth's Crust and Upper Mantle (Paperback, 1971 ed.)
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Deep Seismic Sounding of the Earth's Crust and Upper Mantle (Paperback, 1971 ed.)
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Deep seismiC sounding was proposed by G. A. Gamburtsev and
developed under his guid ance during the period 1948-1955 at the
Institute of Physics of the Earth of the Academy of Sciences of the
USSR. During that period also, the first geophysical results
concerning the deep structure of the earth's crust in several
regions in Tien-Shan, the Pamir, and Turkmenia were observed.
Beginning with 1956, the deep seismic sounding method has been used
widely by geo physical research groups as well as by geophysical
service organizations for regional studies in the USSR.
Descriptions of this work have been given in reports by Yu. N.
Godin, V. V. Fedynskii, D. N. Kazanli, and others. New variants of
the deep seismic sounding method have been developed; continuous
profiling (Yu. N. Godin, and others), and point soundings (N. N.
Puzyrev, and others). Deep seismic soundings have been carried on
outside of Russia also, and studies have been carried out on the
use of the deep seismic sounding method in marine applications (E.
I. Gal'perin, S. M. Zverev, 1. P. Kosminskaya, Yu. P. Neprochnov,
and others). OVer the past decade, the deep seismic sounding method
has joined the suite of geo physical studies as a highly detailed
method for studying the earth's crust and upper mantle to depths of
50 to 100 km on land, and of 15 to 25 km in the deep oceans."
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