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Titlebook: Deep Seismic Sounding of the Earth’s Crust and Upper Mantle; Irina P. Kosminskaya Book 1971 Consultants Bureau, New York 1971 carr.marine.

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书目名称Deep Seismic Sounding of the Earth’s Crust and Upper Mantle
编辑Irina P. Kosminskaya
视频video
图书封面Titlebook: Deep Seismic Sounding of the Earth’s Crust and Upper Mantle;  Irina P. Kosminskaya Book 1971 Consultants Bureau, New York 1971 carr.marine.
描述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 st
出版日期Book 1971
关键词carr; marine; ocean; organization; research; seismic
版次1
doihttps://doi.org/10.1007/978-1-4684-7867-9
isbn_softcover978-1-4684-7869-3
isbn_ebook978-1-4684-7867-9
copyrightConsultants Bureau, New York 1971
The information of publication is updating

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https://doi.org/10.1057/9781403984623s of conditions to be considered: the conditions under which the waves are generated; 2) the conditions prevalent within the medium through which the waves propagate and where they are modified to provide the information of interest; and 3) the conditions under which the waves are detected, and the
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Prayers: Overcoming Fear and Anxiety,ions are usually based, if not always, only on the resultant velocity sections obtained in these areas. Each of these has been constructed on the basis of some arbitrary analysis of the observed features of wave propagation. However, we have not yet closely examined this topic. Moreover, the topic is quite obscure.
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https://doi.org/10.1007/978-90-481-3392-5An examination of the question of the resolution of a seismic method, that is, the degree of detail with which the inhomogeneous velocity structure of a medium may be studied, requires the choice of a schematic model for the medium and its properties.
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