Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Narcea Antiform"'
Autor:
Rubio Ordóñez, Álvaro, Cuesta, Andrés, Gallastegui, G., Suárez Hernando, Oier, Pupin, J. P., Corretgé Castañón, Luis Guillermo
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
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In the Narcea Antiform, both Ediacaran upper volcanic series and volcanic clasts in the overlying Cambrian micro-conglomerates, show geochemistry between those of calc-alkaline and alkaline series in the TAS diagram, and a mainly calc-alkaline trend
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::0c708640473c3eee3e2b66082153a82f
http://hdl.handle.net/10272/8584
http://hdl.handle.net/10272/8584
Detrital minerals provenance studies have become a common tool to decipher paleogeographic scenarios in many orogenic belts. Together with the geochronological single mineral dating, the geochemistry of detrital minerals can provide insights on the s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::9deb2791b3ddaddf5deb35ed92bb08c6
Autor:
Rubio Ordóñez, Álvaro, Cuesta, Andrés, Gallastegui, G., Suárez Hernando, Oier, Pupin, J. P., Corretgé Castañón, Luis Guillermo
In the Narcea Antiform, both Ediacaran upper volcanic series and volcanic clasts in the overlying Cambrian micro-conglomerates, show geochemistry between those of calc-alkaline and alkaline series in the TAS diagram, and a mainly calc-alkaline trend
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::0c708640473c3eee3e2b66082153a82f
https://hdl.handle.net/10272/8584
https://hdl.handle.net/10272/8584
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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GREDOS. Repositorio Institucional de la Universidad de Salamanca
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
GREDOS. Repositorio Institucional de la Universidad de Salamanca
Arias Montano. Repositorio Institucional de la Universidad de Huelva
4 páginas, 2 figuras, 1 tabla.-- Trabajo presentado en la 40ª Sesión Científica, León, 2006.
Detrital minerals provenance studies have become a common tool to decipher paleogeographic scenarios in many orogenic belts. Together with the geoc
Detrital minerals provenance studies have become a common tool to decipher paleogeographic scenarios in many orogenic belts. Together with the geoc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::44af91a17789dc511e7b926f48b9459c
http://hdl.handle.net/10261/28876
http://hdl.handle.net/10261/28876
Autor:
Gutiérrez Alonso, Gabriel, Fernández Suárez, J., Keppie, J. D., Ortega Rivera, M. A., Lee, J. K. W., Murphy, J. B.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Las edades 40Ar/39Ar obtenidas a partir de anfíboles del granitoide Neoproterozoico de Puente de Selce, localizado en el Antiforme del Narcea junto con la existencia de fábricas de deformación relictas generadas en condiciones de media-alta temper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::faa32dd492462e0cfee124a160d96772
http://hdl.handle.net/10272/8687
http://hdl.handle.net/10272/8687
Autor:
Gutiérrez Alonso, Gabriel, Fernández Suárez, J., Keppie, J. D., Ortega Rivera, M. A., Lee, J. K. W., Murphy, J. B.
Las edades 40Ar/39Ar obtenidas a partir de anfíboles del granitoide Neoproterozoico de Puente de Selce, localizado en el Antiforme del Narcea junto con la existencia de fábricas de deformación relictas generadas en condiciones de media-alta temper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::faa32dd492462e0cfee124a160d96772
https://hdl.handle.net/10272/8687
https://hdl.handle.net/10272/8687
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
4 sequence of acid to basic igneous rocks is exposed within Neoproterozoic sediments of the Narcea Antiform (N of the Iberian Variscan Belt). Volcanic and volcanoclastic rocks, classically known as 'porphyroids', are rhyolites to andesites in composi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::900c837bee71f28a104f73ab3abd4ce3
http://hdl.handle.net/10272/8945
http://hdl.handle.net/10272/8945
4 sequence of acid to basic igneous rocks is exposed within Neoproterozoic sediments of the Narcea Antiform (N of the Iberian Variscan Belt). Volcanic and volcanoclastic rocks, classically known as 'porphyroids', are rhyolites to andesites in composi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::900c837bee71f28a104f73ab3abd4ce3
https://hdl.handle.net/10272/8945
https://hdl.handle.net/10272/8945
Autor:
Rubio Ordóñez, Álvaro, Barba, Pedro, Cuesta, Andrés, Gallastegui, G., Suárez Hernando, Oier, Ugidos, José María, Valladares, María Isabel
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
In the East limb of the Narcea Antiform (Iberian massif) outcrops siliciclastic Cambrian materials with uncomformity disposition over the Neoproterozoic Narcea Slates. The lower Cambrian Herrería Fm. in the Cantabrian Zone includes a conglomeratic u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::681be42debf39661f13b19cfc019ecc1
http://hdl.handle.net/10272/8943
http://hdl.handle.net/10272/8943
Autor:
Rubio Ordóñez, Álvaro, Barba, Pedro, Cuesta, Andrés, Gallastegui, G., Suárez Hernando, Oier, Ugidos, José María, Valladares, María Isabel
In the East limb of the Narcea Antiform (Iberian massif) outcrops siliciclastic Cambrian materials with uncomformity disposition over the Neoproterozoic Narcea Slates. The lower Cambrian Herrería Fm. in the Cantabrian Zone includes a conglomeratic u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::681be42debf39661f13b19cfc019ecc1