Electrical Properties of the Earth’s Mantle 1987
DOI: 10.1007/978-3-0348-7373-4_10
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Conductivity Profiles from Global Data

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Cited by 4 publications
(3 citation statements)
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“…This method has been successfully used to infer the electrical conductivity of the Earth (Banks, 1969;Chapman and Price, 1930;Hobbs, 1987;Kuvshinov and Olsen, 2006;Lahiri and Price, 1939;Rikitake, 1966;Roberts, 1986;Schuster, 1889;Tarits, 1994) and the Moon (Schubert and Schwartz, 1969;Sonett, 1982;Sonett et al, 1971). It has also been used to find subsurface liquid salt water oceans on the Galilean satellites Europa, Ganymede, and Callisto (Khurana et al, 1998;Kivelson et al, 1999Kivelson et al, , 2000Kivelson et al, , 2002Kivelson et al, , 2004Zimmer et al, 2000) and a subsurface magma ocean on Io (Khurana et al, 2011).…”
Section: Electromagneticsmentioning
confidence: 99%
“…This method has been successfully used to infer the electrical conductivity of the Earth (Banks, 1969;Chapman and Price, 1930;Hobbs, 1987;Kuvshinov and Olsen, 2006;Lahiri and Price, 1939;Rikitake, 1966;Roberts, 1986;Schuster, 1889;Tarits, 1994) and the Moon (Schubert and Schwartz, 1969;Sonett, 1982;Sonett et al, 1971). It has also been used to find subsurface liquid salt water oceans on the Galilean satellites Europa, Ganymede, and Callisto (Khurana et al, 1998;Kivelson et al, 1999Kivelson et al, , 2000Kivelson et al, , 2002Kivelson et al, , 2004Zimmer et al, 2000) and a subsurface magma ocean on Io (Khurana et al, 2011).…”
Section: Electromagneticsmentioning
confidence: 99%
“…The Parker & Whaler (1981) approximation scheme described in the previous section was applied to some real data to search for a suitable value of N * . This preliminary work was carried out on data from two sources: (i) Hobbs (1987). 8 frequencies considered ranging between 0.094 and 0.750 cycles per day (cpd); (ii) Larsen (1975).…”
Section: Inversion Of Synthetic Modelsmentioning
confidence: 99%
“…It was hoped that such a frequency range would enable the estimation of at least the first few pole locations of the response function. The data were derived using a technique similar to that employed by Hobbs (1987) in the analysis of six magnetic storms considered by Marshall (1980). The results of Marshall, who separated the external and internal field components corresponding to the harmonic n = 1 for each storm at hourly intervals, were taken as the raw data.…”
Section: The Derivation O F a Response Set A N D Its S U B S E Q U E mentioning
confidence: 99%