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estructura gravimétrica y magnética de la corteza del suroeste ...

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Nieves Sánchez Jiménez<br />

CRAWFORD, A. J.; FALLOON, T. J. y GREEN, D. H. (1989): C<strong>la</strong>ssification, petrogenesis<br />

and tectonic setting of boninites. En: Boninites and re<strong>la</strong>ted rocks, (Ed. A. J. Crawford),<br />

Unwin Hyman, Londres, 450 pp.<br />

CRESPO-BLANC, A. (1991): Evolución geotectónica <strong>de</strong>l contacto entre <strong>la</strong> Zona <strong>de</strong> Ossa-<br />

Morena y <strong>la</strong> Zona Surportuguesa en <strong>la</strong>s Sierras <strong>de</strong> Aracena y Aroche (Macizo Ibérico<br />

meridional): Un contacto mayor en <strong>la</strong> Ca<strong>de</strong>na Hercínica Europea. Tesis Doctoral, Univ.<br />

Granada, 329 pp.<br />

CRESPO-BLANC, A. y OROZCO, M. (1988): The Southern Iberian Shear Zone: a major<br />

boundary in the Hercynian fol<strong>de</strong>d belt. Tectonophysics, 148, pp. 221-227.<br />

CHACÓN, J. (1979): Estudio geológico <strong>de</strong>l sector central <strong>de</strong>l anticlinorio Portoalegre-<br />

Badajoz-Córdaba (SW <strong>de</strong>l Macizo Ibérico). Tesis Doctoral, Univ. <strong>de</strong> Granada, 721 pp.<br />

CHACÓN, J. y PASCUAL, E. (1977): El anticlinorio Portoalegre-Badajoz-Córdoba<br />

divisoria entre <strong>la</strong>s zonas Centro Ibérica y Ossa-Morena (Sector SW <strong>de</strong>l Macizo Ibérico).<br />

Cuad. Geol. Univ. Granada, 8-9, pp. 21-35.<br />

CHACÓN, J.; DELGADO-QUESADA, M. y GARROTE, A. (1974): Sobre <strong>la</strong> existencia <strong>de</strong><br />

dos diferentes dominios <strong>de</strong> metamorfismo regional en <strong>la</strong> banda Elvas-Badajoz-Córdoba<br />

(Macizo Hespérico Meridional). Bol. Geol. Min., 85, 6, pp. 713-717.<br />

CHACÓN, J.; OLIVEIRA, V.; RIBEIRO, A. y OLIVEIRA, J. T. (1983): La <strong>estructura</strong> <strong>de</strong> <strong>la</strong><br />

Zona <strong>de</strong> Ossa-Morena. En: Libro Jubi<strong>la</strong>r J. M. Ríos. Geología <strong>de</strong> España, (Ed. J. A.<br />

Comba), Tomo 1, IGME, pp. 490-504.<br />

CHAKRABORTY, K. y AGARWAL, B. N. P. (1992): “Mapping of crustal discontinuities<br />

by wavelength filtering of the gravity field”. Geophysical Prospecting, 41, pp. 801-822.<br />

CHIAN, D. y LOUDEN, K. E. (1994): The continent-ocean crustal transition across the<br />

southwest Green<strong>la</strong>nd margin. Journal of Geophysical Research, 99, B5, pp. 9117-9135.<br />

CHIAN, D.; LOUDEN, K. E. y REID, I. (1995): Crustal structure of the Labrador Sea<br />

conjugate margin and implications for the formation of nonvolcanic continental margins.<br />

Journal of Geophysical Research, 100, B12, pp. 24239-24253.<br />

CHRISTENSEN, N. I. y FOUNTAIN, D. M. (1975): Constitution of the lower continental<br />

crust based on experimental studies of seismic velocities in granulites. Geological Society of<br />

America Bulletin, 86, pp. 227-236.<br />

CHRISTENSEN, N. I. y SHAW, G. H. (1970): E<strong>la</strong>sticity of mafic rocks from the mid-<br />

At<strong>la</strong>ntic ridge. Geophys. J. R. Astron. Soc., 20, pp. 271-284.<br />

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