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Titlebook: Geoelectromagnetic Investigation of the Earth’s Crust and Mantle; Igor I. Rokityansky Book 1982 Springer-Verlag Berlin Heidelberg 1982 Erd

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書目名稱Geoelectromagnetic Investigation of the Earth’s Crust and Mantle
編輯Igor I. Rokityansky
視頻videohttp://file.papertrans.cn/384/383136/383136.mp4
圖書封面Titlebook: Geoelectromagnetic Investigation of the Earth’s Crust and Mantle;  Igor I. Rokityansky Book 1982 Springer-Verlag Berlin Heidelberg 1982 Erd
描述Electrical conductivity is a parameter which characterizes composition and physical state of the Earth‘s interior. Studies of the state equations of solids at high temperature and pressure indicate that there is a close relation be- tween the electrical conductivity of rocks and temperature. Therefore, measurements of deep conductivity can provide knowledge of the present state and temperature of the Earth‘s crust and upper mantle matter. Infor- mation about the temperature of the Earth‘s interior in the remote past is derived from heat flow data. Experimental investigation of water-containing rocks has revealed a pronounced increase of electrical conductivity in the temperature range D from 500 to 700 DC which may be attributed to the beginning of fractional melting. Hence, anomalies of electrical conductivity may be helpful in identitying zones of melting and dehydration. The studies of these zones are perspective in the scientific research of the mobile areas of the Earth‘s crust and upper mantle where tectonic movements, processes ofthe region- al metamorphism and of forming mineral deposits are most intensive. Thus, in the whole set of research on physics of the Earth the stud
出版日期Book 1982
關(guān)鍵詞Erdkruste; Erdmantel; Geoelektrik; aurora; identity; magnetic field; metamorphism; mineral; mineral deposits
版次1
doihttps://doi.org/10.1007/978-3-642-61801-7
isbn_softcover978-3-642-61803-1
isbn_ebook978-3-642-61801-7
copyrightSpringer-Verlag Berlin Heidelberg 1982
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Geoelectromagnetic Fields, followed by consideration of the origin of the main variations and pulsations, the effect of conductive excitation of the variations due to atmospheric vertical currents is discussed. This chapter is primarily intended to provide the basis for constructing models of electromagnetic field sources employed in deep geoelectrics.
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Book 1982olids at high temperature and pressure indicate that there is a close relation be- tween the electrical conductivity of rocks and temperature. Therefore, measurements of deep conductivity can provide knowledge of the present state and temperature of the Earth‘s crust and upper mantle matter. Infor-
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https://doi.org/10.1007/978-3-658-20113-5ed Earth to an external electromagnetic field, taken in the form of a spherical (plane) harmonic, are described in the third section. The last section outlines the basic mathematical models applied for describing real geoelectric structures.
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Elements of the Theory of Electromagnetic Fields,ions which relate fields and their potentials to the sources, such as electric and magnetic currents. In the second section electric and magnetic fields induced within horizontally layered Earth are being expanded in a series in spherical (and plane) harmonics. Functions of the response of the layer
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