Lateral heterogeneities in the upper and mid-mantle conductivity in Argentina

Regional studies of Sq variations measured at five permanent observatories in Argentina were performed to estimate the distribution of the electrical conductivity of the upper and mid-mantle, reaching a depth of approximately 800 km. After separating the total field into its parts of external and in...

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Detalles Bibliográficos
Autor principal: Osella, A.
Otros Autores: Favetto, Alicia Beatriz, Martinelli, P.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: Birkhäuser-Verlag 1993
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Acceso en línea:Registro en Scopus
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Registro en la Biblioteca Digital
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100 1 |a Osella, A. 
245 1 0 |a Lateral heterogeneities in the upper and mid-mantle conductivity in Argentina 
260 |b Birkhäuser-Verlag  |c 1993 
270 1 0 |m Osella, A.; Departmento de Física Facultad de Ciencias, Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pab. 1, Buenos Aires, 1428, Argentina 
504 |a Berdichevsky, M., Zhdanov, M., (1984) Advanced Theory of Deep Geomagnetic Sounding, , Elsevier, N.Y 
504 |a Campbell, W.H., Schiffmacher, E.R., Upper Mantle Electrical Conductivity for Seven Subcontinental Regions of the Earth (1988) J. Geomag. Geoelectr., 40, pp. 1387-1406 
504 |a Everett, J.E., Hyndman, R.D., Geomagnetic Variations and Electrical Conductivity Structure in Southern Australia (1967) Phys. Earth Planet. Int., 1, pp. 24-34 
504 |a Jupp, D.L.B., Vozoff, K., Stable Iterative Methods for the Inversion of Geophysical Data (1975) Geophys. J. R. Astr. Soc., 42 (3), pp. 957-976 
504 |a Matsushita, S., Maeda, H., On the Geomagnetic Solar Quiet Daily Variation Field during the IGY (1965) J. Geophys. Res., 70 (11), pp. 315-338 
504 |a Osella, A.M., Duhau, S., The Effect of the Depth of the Nonconducting Layer on the Induced Magnetic Field at the Peruvian Dip Equator (1983) J. Geomag. Geoelectr., 35, p. 245 
504 |a Osella, A. M., Favetto, A., and Martinelli, P. (1992), Sensitivity of the Geomagnetic Daily Variations to 2D Structures, Trends in Geophysics (in press); Osella, A. M., Favetto, A., and Van Zele, A. (1993a), Spectral Analysis of Geomagnetic Variations at Equatorial and Mid-latitudes, Geoacta (in press); Osella, A.M., Martinelli, P., Magnetotelluric Responses of Anisotropic Bidimensional Structures (1993) Geophys. J. Int., 115, pp. 819-828 
504 |a Osella, A. M., Pomposiello, C., Favetto, A., Sainato, C., and Martinelli, P. (1993b), Bidimensional Modeling of a Geothermal Anomaly in the Eastern Border of Aconquija Range, Acta Geod. Geophys. Mount. (in press); Schmucker, U., Anomalies of Geomagnetic Variations in the Southwestern United States (1964) Journal of geomagnetism and geoelectricity, 15, pp. 193-221 
504 |a Schultz, A., Larsen, J.C., On the Electrical Conductivity of the Mid-mantle. I. Calculation of Equivalent Scalar Magnetotelluric Response Functions (1987) Geophys. J. R. Astr. Soc., 88, pp. 733-761 
506 |2 openaire  |e Política editorial 
520 3 |a Regional studies of Sq variations measured at five permanent observatories in Argentina were performed to estimate the distribution of the electrical conductivity of the upper and mid-mantle, reaching a depth of approximately 800 km. After separating the total field into its parts of external and internal origin, the in duced field was modeled, applying two-dimensional techniques. Additionally, induction arrows and an equivalent apparent resistivity curve were calculated A north-south heterogeneity was detected, showing an increase of the conductivity of the shallower layers north of the profile, which may be related to the presence of high volcanic activity in the area. © 1993 Birkhäuser Verlag.  |l eng 
593 |a Departmento de Física Facultad de Ciencias, Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pab. 1, Buenos Aires, 1428, Argentina 
651 4 |a MANTLE CONDUCTIVITY IN ARGENTINA 
690 1 0 |a LATERAL ELECTRICAL HETEROGENEITIES 
690 1 0 |a SQ FIELD 
700 1 |a Favetto, Alicia Beatriz 
700 1 |a Martinelli, P. 
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