Present-day strain field on the South American slab underneath the Sandwich Plate (Southern Atlantic Ocean): a kinematic model

Autor: J. J. Martínez-Díaz, Raúl Pérez-López, J. M. González-Casado, Miguel Ángel Rodríguez-Pascua, Jorge Luis Giner Robles

Publikováno v: Geological Society, London, Special Publications. 328:155-167

This work analyses the present-day principal strain orientation on the downgoing slab of the South America Plate (SAM) beneath the Sandwich Plate (SAND). The strain regime was deduced from the study of 331 earthquake focal mechanism solutions examine

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::21bc988e7d78fd2d7ef57d78345011aa
https://doi.org/10.1144/sp328.6

Revisión de la zonación metamórfica y los procesos de blastesis-deformación de la región de Somosierra (Sistema Central Español)

Autor: J. M. González Casado

Publikováno v: Estudios Geologicos, Vol 43, Iss 3-4, Pp 209-216 (1987)

En un área comprendida entre el plutón de La Cabrera y el macizo de Honrubia, se han estudiado las asociaciones minerales en metapelitas y venas de segregación de cuarzo, las zonaciones metamórficas propuestas se relacionan espacialmente con una

Externí odkaz: https://doaj.org/article/ac9f142f616b47e483aecc364e401316

Cenozoic thick-skinned deformation and topography evolution of the Spanish Central System

Autor: A. Olaiz, G. de Vicente, Paul Andriessen, P.G. Silva, A. Muñoz Martín, Sierd Cloetingh, J. Álvarez, J.D. van Wees, A. Carbó, J. M. González Casado, Ramón Vegas

Publikováno v: Global and Planetary Change, 58(1-4), 335-382. Elsevier
de Vincente, G, Vegas, R, Munoz Martin, A, Silva, P G, Andriessen, P A M, Cloetingh, S A P L, Gonzalez Casado, J M, van Wees, J D A M, Alvarez, J, Carbo, A & Olaiz, A 2007, ' Cenozoic thick-skinned deformation and topography evolution of the Spanish Central System ', Global and Planetary Change, vol. 58, no. 1-4, pp. 335-382 . https://doi.org/10.1016/j.gloplacha.2006.11.042
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname

The Spanish Central System is a Cenozoic pop-up with an E-W to NE-SW orientation that affects all the crust (thick-skinned tectonics). It shows antiform geometry in the upper crust with thickening in the lower crust. Together with the Iberian Chain i

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2a24a0770620851cfc3b101b883dd4dd
https://research.vu.nl/en/publications/9c5fa277-9083-4cd3-866d-ebffc4c86c90

Retrograde evolution of quartz segregations from the Dos Picos shear zone in the Nevado-Filabride Complex (Betic chains, Spain). Evidence from fluid inclusions and quartz c-axis fabrics

Autor: J. M. González-Casado, César Casquet, José Miguel Martínez-Martínez, Víctor García-Dueñas

Publikováno v: Geologische Rundschau. 84

Synkinematic quartz veins are ubiquitous in the shear zone separating the Veleta unit from the Calar Alto unit in the internal part of the Betic Cordilleras. They have been studied with respect to quartz c-axis fabrics, microstructures and fluid incl

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::833b70791eb783715a0e6bba59f1b297
https://doi.org/10.1007/bf00192249