Orientaciones ópticas del cuarzo en relación con la zona de cizalla de Berzosa-Honrubia (Sistema Central Español)

Autor: J. M. González Casado

Publikováno v: Estudios Geologicos, Vol 42, Iss 6, Pp 433-438 (1986)

Se estudian las orientaciones ópticas del cuarzo, en las venas de segregación de cuarzo y cuarcitas, que afloran en la región de Somosierra (Sistema Central Español). Se observa como las fábricas reflejan dos tipos de deformaciones, unas por ciz

Externí odkaz: https://doaj.org/article/f575c71bd5e3469390f9e643da220c39

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

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
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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