Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Larrea Bilbao, F. J."'
Autor:
García de Madinabeitia, S., Santos Zalduegui, José Francisco, Larrea Bilbao, F. J., Carracedo Sánchez, Manuel, Gil Ibarguchi, José Ignacio
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
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New lead Isotope results for twenty-four galenas of the Linares-La Carolina mining district (Jaén, Spain) are reported. While two.mineralization types, one near Linares (where filons with low Ag content crosscut the Linares and/or Guadalén-Arquillo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::af6fde477b246f78bab52584abdd95d2
http://hdl.handle.net/10272/9043
http://hdl.handle.net/10272/9043
Autor:
García de Madinabeitia, S., Santos Zalduegui, José Francisco, Larrea Bilbao, F. J., Carracedo Sánchez, Manuel, Gil Ibarguchi, José Ignacio
New lead Isotope results for twenty-four galenas of the Linares-La Carolina mining district (Jaén, Spain) are reported. While two.mineralization types, one near Linares (where filons with low Ag content crosscut the Linares and/or Guadalén-Arquillo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::af6fde477b246f78bab52584abdd95d2
https://hdl.handle.net/10272/9043
https://hdl.handle.net/10272/9043
Autor:
García de Madinabeitia, S., Santos Zalduegui, José Francisco, Carracedo Sánchez, Manuel, Larrea Bilbao, F. J.
We report the results of Pb isotope analyses on representative galena samples from the El Zumajo quartz-rich dyke. This is a late intrusion within the Cardeha-Virgen de La Cabeza granite of the Los Pedroches Hercynian batholith. The batholith granodi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::9ca9fc07c9d3c5479f73705ed1087cf5
Autor:
Jiménez, R., Carracedo Sánchez, Manuel, Ortega, Luis Ángel, Larrea Bilbao, F. J., Alonso Olazabal, Ainhoa
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Los Pedroches batholith (Iberian Massif, SW Spain) is composed by a large granodioritic intrusion and smaller monzogranitic plutons. This batholith is cross cut by a dyke complex of lamprophyres, trachyandesites, dacites, aplites, aplopegmatites,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::0ab8c6eb6f59c12bb1fafebae53985d7
http://hdl.handle.net/10272/9518
http://hdl.handle.net/10272/9518
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Cardena-Virgen de La Cabeza pluton is an high-K peraluminous granitoid wich forms a part ot the Los Pedroches batholith (Central Iberian Zone). Taking account the chemical features of its major elements and comparing with some experimental melts,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::2588f9746b36f0c4b0beeed18a267138
http://hdl.handle.net/10272/9520
http://hdl.handle.net/10272/9520
The Cardena-Virgen de La Cabeza pluton is an high-K peraluminous granitoid wich forms a part ot the Los Pedroches batholith (Central Iberian Zone). Taking account the chemical features of its major elements and comparing with some experimental melts,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::2588f9746b36f0c4b0beeed18a267138
https://hdl.handle.net/10272/9520
https://hdl.handle.net/10272/9520
Autor:
Jiménez, R., Carracedo Sánchez, Manuel, Ortega, Luis Ángel, Larrea Bilbao, F. J., Alonso Olazabal, Ainhoa
The Los Pedroches batholith (Iberian Massif, SW Spain) is composed by a large granodioritic intrusion and smaller monzogranitic plutons. This batholith is cross cut by a dyke complex of lamprophyres, trachyandesites, dacites, aplites, aplopegmatites,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::0ab8c6eb6f59c12bb1fafebae53985d7
Autor:
Larrea Bilbao, F. J., Carracedo Sánchez, Manuel, Tubía, José María, Aranguren, A., Cuevas, Julia
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The northern edge of Los Pedroches granodioritic pluton is deformed by the Conquista fault, a right ductile shear zone with a normal component. Consecuently, the rocks of this sector show gradual texture-structural modifications, without any differen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::dfea69f574cc1992e4c61f4e027e2c2f
http://hdl.handle.net/10272/9515
http://hdl.handle.net/10272/9515
Autor:
Larrea Bilbao, F. J., Carracedo Sánchez, Manuel, Tubía, José María, Aranguren, A., Cuevas, Julia
The northern edge of Los Pedroches granodioritic pluton is deformed by the Conquista fault, a right ductile shear zone with a normal component. Consecuently, the rocks of this sector show gradual texture-structural modifications, without any differen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::dfea69f574cc1992e4c61f4e027e2c2f
https://hdl.handle.net/10272/9515
https://hdl.handle.net/10272/9515
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
This paper is a brief description of the Hercynian calc-alkaline granodioritic pluton of the Los Pedroches batholith at its NW branch (La Serena, Badajoz). This study is located in the National Topographic Map N.T.M. number 805 of Castuera, and it ta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::7bbde22eb6459c578c6b156f365fe940
http://hdl.handle.net/10272/10526
http://hdl.handle.net/10272/10526