Electrical and thermal anomalies in the central andean subduction zone
An enhancement of the electrical conductivity in the upper layers in the subduction zones of southern Peru and northern Argentina is found by analyzing the solar quiet geomagnetic variations. This feature appears in a zone associated with large subduction angles. In this region high values of heat f...
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Formato: | Capítulo de libro |
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Birkhauser Verlag AG
1997
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001 | PAPER-20101 | ||
003 | AR-BaUEN | ||
005 | 20250313083952.0 | ||
008 | 190411s1997 xx ||||fo|||| 00| 0 eng|d | ||
024 | 7 | |2 scopus |a 2-s2.0-0030744957 | |
040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
100 | 1 | |a Favetto, Alicia Beatriz | |
245 | 1 | 0 | |a Electrical and thermal anomalies in the central andean subduction zone |
260 | |b Birkhauser Verlag AG |c 1997 | ||
270 | 1 | 0 | |m Favetto, A.; Dep. de Fis.-Fac. Cs. Exactas, Universidad de Buenos Aires, Ciudad Universitaria, Pab 1, 1428 Buenos Aires, Argentina |
504 | |a Allmendinger, R., Figueroa, D., Snyder, E., Beer, J., Mpodozis, C., Isacks, B.L., Foreland Shortening and Crustal Balancing in the Andes at 30° Latitude (1990) Tectonics, 9, pp. 789-809 | ||
504 | |a Assumpçao, M., The Regional Intraplate Stress Field in South America (1992) J. Geophys. Res., 97, pp. 11889-11903 | ||
504 | |a Barazangi, M., Isacks, B., Spatial Distribution of Earthquakes and Subduction of the Nazca Plate beneath South America (1976) Geology, 4, pp. 686-692 | ||
504 | |a Cahill, T., Isacks, B., Seismicity and Shape of the Subducted Nazca Plate (1992) J. Geophys. Res., 97, pp. 17503-17529 | ||
504 | |a Campbell, W., Schiffmacher, E., Upper Mantle Electrical Conductivity for Seven Subcontinental Regions of the Earth (1988) J. Geomag. Geoelectr., 40, pp. 1387-1406 | ||
504 | |a Chapman, D.S., Pollack, H.N., Regional Geotherms and Lithospheric Thickness (1977) Geology, 5, pp. 265-268 | ||
504 | |a Dorbath, C., Garnet, M., Poupinet, G., Martinez, C., A Teleseimic Study of the Altiplano and Eastern Cordillera in Northern Bolivia: New Constraints on a Lithopheric Model (1993) J. Geophys. Res., 98, pp. 9825-9844 | ||
504 | |a Fukao, Y., Yamamoto, A., Kono, M., Gravity Anomaly across the Peruvian Andes (1989) J. Geophys. Res., 94, pp. 3867-3890 | ||
504 | |a Giese, P., Geothermal structure of the Central Andean crust - Implications for heat transport and rheology (1993) Tectonics of the Southern Central Andes, pp. 69-76. , (eds. Reutter, K. J., Scheuber, E., and Wigger, P. J.) Springer-Verlag, New York | ||
504 | |a Henry, S.G., Pollack, H.N., Terrestrial Heat Flow above the Andean Subduction Zone in Bolivia and Peru (1988) J. Geophys. Res., 93, pp. 15153-15162 | ||
504 | |a James, D.E., Andean Crustal and Upper Mantle Structure (1971) J. Geophys. Res., 76, pp. 3246-3271 | ||
504 | |a James, D.E., Snoke, J.A., Structure and Tectonics in the Region of the Flat Subduction beneath Central Peru: Crust and Uppermost Mantle (1994) J. Geophys. Res., 99, pp. 6899-6912 | ||
504 | |a Jordan, T.E., Isacks, B.L., Allmendinger, R.W., Brewer, J.A., Ramos, V.A., Ando, C.L., Andean Tectonics Related to Geometry of Subducted Nazca Plate (1983) Geol. Soc. Am. Bull., 94, pp. 341-361 | ||
504 | |a Norabuena, E.O., Snoke, A., James, D., Structure of the Subducting Nazca Plate beneath Peru (1994) J. Geophys Res, 99, pp. 9215-9226 | ||
504 | |a Osella, A.M., Favetto, A., Martinelli, P., Lateral Heterogeneities in the Upper and Mid-mantle Conductivity in Argentina (1993) Pure and Appl. Geophys., 141, pp. 139-156 | ||
504 | |a Osella, A.M., Favetto, A., Martinelli, P., Sensitivity of the Geomagnetic Daily Variations to 2D Structures (1993) Trends in Geophys. Res., 2, pp. 141-155 | ||
504 | |a Peacock, S.M., Thermal Effect of Metamorphic Fluids in Subduction Zones (1987) Geology, 15, pp. 1057-1060 | ||
504 | |a Schmitz, M., A Balanced Model of the Southern Central Andes (1994) Tectonics, 13 (2), pp. 485-492 | ||
504 | |a Schmucker, U., Hartmann, O., Giesecke, A.A., Casaverde, M., Forbush, S.E., Electrical Conductivity in the Earth's Crust in Peru (1963) Carnegie Institution of Washington Yearbook, 63, pp. 354-362 | ||
504 | |a Sheffels, B., Lower Bound on the Amount of Crustal Shortening in the Central Bolivian Andes (1990) Geology, 18, pp. 812-815 | ||
504 | |a Smalley, R., Pujol, J., Regnier, M., Chiu, J.M., Chatelain, B.L., Araujo, M., Puebla, N., Basement Seismicity beneath the Andean Precordillera Thin-skinned Thrust Belt and its Implications for Crustal and Lithosphere Behavior (1993) Tectonics, 12, pp. 63-76 | ||
504 | |a Tarits, P., Menvielle, M., The Andean Conductivity Anomaly Reexamined (1986) Annales Geophysicae, 4 B, pp. 63-70 | ||
504 | |a Whitman, D., Moho Geometry beneath the Eastern Margin of the Andes, Northwest Argentina, and its Implications to the Effective Elastic Thickness of the Andean Foreland (1994) J. Geophys. Res., 99, pp. 15277-15289 | ||
504 | |a Wigger, P., Schmitz, M., Araneda, M., Asch, G., Baldzhun, S., Giese, P., Heinsohn, W.D., Viramonte, J., Variation of the crustal structure of the southern Central Andes deduced from seismic refraction investigations (1993) Tectonics of the Southern Central Andes, pp. 23-48. , (eds. Reutter, K. J., Scheuber, E., and Wigger, P. J.) Springer-Verlag, New York | ||
506 | |2 openaire |e Política editorial | ||
520 | 3 | |a An enhancement of the electrical conductivity in the upper layers in the subduction zones of southern Peru and northern Argentina is found by analyzing the solar quiet geomagnetic variations. This feature appears in a zone associated with large subduction angles. In this region high values of heat flow have been measured, therefore a one-dimensional thermal model is proposed using regional characteristic parameters to reproduce these values. It is found that thermal convection necessarily plays a contributing role. This effect may be produced by the ascending magma and fluids, which can explain the enhancement of the electrical conductivity. |l eng | |
536 | |a Detalles de la financiación: Fundación Antorchas | ||
536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
536 | |a Detalles de la financiación: This work was partly supported by CONICET (Consejo Nacional de Investiga-ciones Científicas y Técnicas) and Fundación Antorchas. | ||
593 | |a Dep. de Fis.-Fac. Cs. Exactas, Universidad de Buenos Aires, Ciudad Universitaria, Pab 1, 1428 Buenos Aires, Argentina | ||
593 | |a CONICET, Argentina | ||
651 | 4 | |a SOUTH AMERICA, ANDES | |
690 | 1 | 0 | |a CENTRAL ANDES |
690 | 1 | 0 | |a ELECTRICAL ANOMALY |
690 | 1 | 0 | |a THERMAL ANOMALY |
690 | 1 | 0 | |a ELECTRICAL CONDUCTIVITY |
690 | 1 | 0 | |a HEAT FLOW |
690 | 1 | 0 | |a SUBDUCTION ZONE |
690 | 1 | 0 | |a THERMAL ANOMALY |
700 | 1 | |a Martinelli, P. | |
700 | 1 | |a Osella, A. | |
773 | 0 | |d Birkhauser Verlag AG, 1997 |g v. 149 |h pp. 391-404 |k n. 2 |p Pure Appl. Geophys. |x 00334553 |w (AR-BaUEN)CENRE-86 |t Pure and Applied Geophysics | |
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