Resultats globals: 4 registres trobats en 0.02 segons.
Articles, 4 registres trobats
Articles 4 registres trobats  
1.
18 p, 2.9 MB Evidence of extensional metamorphism associated to Cretaceous rifting of the North-Maghrebian passive margin : the Tanger- Ketama Unit (External Rif, northern Morocco) / Vázquez, M. (Universidad de Chile. Andean Geothermal Center of Excellence (CEGA)) ; Asebriy, L. (Université Mohammed V. Institut Scientifique) ; Azdimousa, A. (Université Mohammed I. Laboratoire LGA) ; Jabaloy, A. (Universidad de Granada. Departamento de Geodinámica) ; Booth-Rea, G. (Universidad de Granada. Departamento de Geodinámica) ; Barbero, L. (Universidad de Cádiz. Departamento de Ciencias de la Tierra) ; Mellini, M. (Università di Siena. Dipartimento di Scienze della Terra) ; González-Lodeiro, F. (Universidad de Granada. Departamento de Geodinámica) ; Consejo Superior de Investigaciones Científicas (Espanya). Instituto Andaluz de Ciencias de la Tierra
The distribution pattern of diagenetic conditions to very low-grade metamorphism in the eastern Rif has been determined based on a study of clay-mineral assemblages and illite crystallinity of Mesozoic metapelites. [...]
2013 - 10.1344/105.000001843
Geologica acta, Vol. 11, Núm. 3 (September 2013) , p. 277-293  
2.
10 p, 1.1 MB From strike-slip to reverse reactivation : the Crevillente Fault System and seismicity in the Bullas-Mula area (Betic Cordillera, SE Spain) / Sanz de Galdeano, C. (Universidad de Granada. Facultad de Ciencias) ; Buforn, E. (Universidad Complutense e Madrid. Departamento de Geofísica y Meteorología) ; Consejo Superior de Investigaciones Científicas (Espanya). Instituto Andaluz de Ciencias de la Tierra
Several major N80ºE faults occur in the Bullas-Mula area (SE Spain). These faults and the numerous thrust slices of the Sierra de Ricote can be related to the movements of the Crevillente (or Cadiz-Alicante) fault system, which causes the westward displacement of the Betic Internal Zone and part of the External Zone. [...]
2005 - 10.1344/105.000001394
Geologica acta, Vol. 3, Núm. 3 (2005) , p. 241-250  
3.
9 p, 287.1 KB Exotic accessory minerals in layered chromitites of the Campo Formoso complex (Brazil) / Zaccarini, F. (University of Leoben. Department of Applied Geological Sciences and Geophysics) ; Garuti, G. (University of Modena and Reggio Emilia. Dipartimento di Scienze della Terra) ; Martin, R. F. (McGill University. Department of Earth and Planetary Sciences) ; Instituto Andaluz de Ciencias de la Tierra
The Campo Formoso stratiform intrusive complex, in Bahia State, Brazil, considered to be of Paleoproterozoic age, consists of a tabular body of ultramafic rocks about 40 km long and 100-1100 m wide. Thick horizons of chromitite are exploited and the deposits are the richest in Brazil. [...]
2006 - 10.1344/105.000000347
Geologica acta, Vol. 4, Núm. 4 (2006) , p. 461-469  
4.
13 p, 572.9 KB Combined use of the GGSFT data base and on board marine collected data to model the Moho beneath the Powell Basin, Antarctica / Chávez Segura, René (Universidad Nacional Autónoma de México. Instituto de Geofísica) ; Flores Márquez, Elsa Leticia (Universidad Nacional Autónoma de México. Instituto de Geofísica) ; Suriñach Cornet, Emma (Universitat de Barcelona. Departament de Geodinàmica i Geofisica) ; Galindo Zaldívar, Jesús (Universidad de Granada. Departamento de Geodinámica) ; Rodríguez Fernández, José (Universidad de Granada) ; Maldonado, Andrés (Universidad de Granada) ; Consejo Superior de Investigaciones Científicas (Espanya). Instituto Andaluz de Ciencias de la Tierra
The Powell Basin is a small oceanic basin located at the NE end of the Antarctic Peninsula developed during the Early Miocene and mostly surrounded by the continental crusts of the South Orkney Microcontinent, South Scotia Ridge and Antarctic Peninsula margins. [...]
2007 - 10.1344/105.000000293
Geologica acta, Vol. 5, Núm. 4 (2007) , p. 323-335  

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