Zobrazeno 1 - 10
of 57
pro vyhledávání: '"A. Díaz de Federico"'
Publikováno v:
Estudios Geologicos, Vol 63, Iss 2, Pp 19-40 (2007)
En este trabajo se muestra la distribución espacial de las diferentes formaciones geológicas que forman los Complejos del Veleta y del Mulhacén en el en el Espacio Natural de Sierra Nevada y se ilustran, mediante fotos macroscópicas y microscópi
Externí odkaz:
https://doaj.org/article/4b839dc0f9224aae98b25840e3724376
Autor:
E. PUGA, L. BECCALUVA, G.L. BIANCHINI, A. DÍAZ DE FEDERICO, M.A. DÍAZ PUG, A.M. ÁLVAREZ VALERO, J. GALINDO ZALDÍVAR, J.R. WIJBRANS
Publikováno v:
Geologica Acta, Vol 8, Iss 2 (2010)
Two drillings carried out at Cerro Prieto (Province of Málaga), together with additional geophysical data, revealed the existence of an igneous body formed of rock-types previously unknown in the Subbetic zone. The recovered rocks, emplaced under hy
Externí odkaz:
https://doaj.org/article/5ec5e53153f84636b7e26b13adc7c521
Autor:
Galindo‐Zaldívar, Jesús, Puga, Encarnación, Bohoyo, Fernando, González, Francisco Javier, Maldonado, Andrés, Martos, Yasmina M., Pérez, Lara F., Ruano, Patricia, Schreider, Anatoly A., Somoza, Luis, Suriñach, Emma, Antonio, Díaz de Federico
Publikováno v:
In Global and Planetary Change December 2014 123 Part B:249-268
Autor:
Galindo‐Zaldívar, Jesús, Puga, Encarnación, Bohoyo, Fernando, González, Francisco Javier, Maldonado, Andrés, Martos, Yasmina M., Pérez, Lara F., Ruano, Patricia, Schreider, Anatoly A., Somoza, Luis, Suriñach, Emma, Antonio, Díaz de Federico
Publikováno v:
In Global and Planetary Change November 2014 122:50-69
Autor:
Jesús Galindo‐Zaldívar, Encarnación Puga, Fernando Bohoyo, Francisco Javier González, Andrés Maldonado, Yasmina M. Martos, Lara F. Pérez, Patricia Ruano, Anatoly A. Schreider, Luis Somoza, Emma Suriñach, Díaz de Federico Antonio
Publikováno v:
Global and Planetary Change. 123:249-268
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f4ac568487d1f3259eadf23503322e9
https://doi.org/10.1016/j.gloplacha.2014.11.002
https://doi.org/10.1016/j.gloplacha.2014.11.002
Autor:
José Antonio Lozano, Antonio Díaz de Federico, Mark Fanning, Luigi Beccaluva, E. Puga, José Miguel Nieto, Gianluca Bianchini, Miguel Angel Díaz Puga, Claudio Natali, José Ángel Rodríguez Martínez-Conde
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
riUAL. Repositorio Institucional de la Universidad de Almería
Universidad de Almería
Digital.CSIC. Repositorio Institucional del CSIC
Digibug. Repositorio Institucional de la Universidad de Granada
instname
riUAL. Repositorio Institucional de la Universidad de Almería
Universidad de Almería
Digital.CSIC. Repositorio Institucional del CSIC
Digibug. Repositorio Institucional de la Universidad de Granada
The Betic Ophiolites consist of numerous tectonic slices, metric to kilometric in size, of eclogitized mafic and ultramafic rocks associated to oceanic metasediments, deriving from the Betic oceanic domain. The outcrop of these ophiolites is aligned
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3f13a25c04b1a88f5ac4f2ebe8b24600
Autor:
Francisco Javier González, Andrés Maldonado, E. Puga, Yasmina M. Martos, A. A. Schreider, Lara F. Pérez, Patricia Ruano, Emma Suriñach, Jesús Galindo-Zaldívar, Luis Somoza, Fernando Bohoyo, Díaz de Federico Antonio
Publikováno v:
Global and Planetary Change. 122:50-69
Dove Basin is situated in the south-central Scotia Sea, between Pirie and Bruce banks, and was formed during the development of the Scotia Arc. The basin has a roughly sigmoidal shape, with a prominent NNE–SSW elongated ridge located in its central
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f28a57f52def9a9205fec12a0e73e5f
https://doi.org/10.1016/j.gloplacha.2014.07.021
https://doi.org/10.1016/j.gloplacha.2014.07.021
Publikováno v:
In LITHOS 1999 49(1):23-56
Autor:
Gianluca Bianchini, Mark Fanning, José Miguel Nieto, Luigi Beccaluva, Antonio Díaz de Federico, E. Puga, Miguel Angel Díaz Puga
Publikováno v:
Lithos. 124:255-272
The Betic Ophiolitic Unit, part of the Mulhacen Complex in the Betic Cordillera (SE Spain), is composed of several tectonic slices of eclogitized mafic and ultramafic rocks, together with oceanic metasediments. A comprehensive review of the petrologi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::430b8a422de5a94094df39498470f70e
https://doi.org/10.1016/j.lithos.2011.01.002
https://doi.org/10.1016/j.lithos.2011.01.002
Publikováno v:
Estudios Geologicos, Vol 63, Iss 2, Pp 19-40 (2007)
We show the spatial distribution of the various geological formations that make up the Veleta and Mulhacén Complexes into the Sierra Nevada Park and illustrate, with macro- and microscopic photographs, their most characteristic types of rock. The Ve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doajarticles::c4bf589938499cb57587268eceefb8d5
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/199/199
http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/199/199