Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Andrés Gil-Imaz"'
Autor:
André Pouclet, J. Javier Álvaro, Jacques-Marie Bardintzeff, Andrés Gil Imaz, Eric Monceret, Daniel Vizcaïno
Publikováno v:
Geoscience Frontiers, Vol 8, Iss 1, Pp 25-64 (2017)
The Cambrian–lower Ordovician volcanic units of the South Armorican and Occitan domains are analysed in a tectonostratigraphic survey of the French Variscan Belt. The South Armorican lavas consist of continental tholeiites in middle Cambrian–Furo
Externí odkaz:
https://doaj.org/article/467a83b89268408a9c6e522407704b23
A sill covering an area of more than 15 km2, several dykes up to 5 m thick and a volcanoclastic deposit crop out with similar petrology in the sector of Atienza (NW Iberian Chain, Spain). They consist of calc-alkaline porphyritic andesites with pheno
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::28a309f5d47aaa62154abb2ff94cde02
http://hdl.handle.net/10810/61088
http://hdl.handle.net/10810/61088
Autor:
Teresa Román-Berdiel, Belén Oliva-Urcia, Antonio M. Casas-Sainz, Pablo Calvín, Bennacer Moussaid, Ruth Soto, Marcos Marcén, Hmidou El-Ouardi, Andrés Pocoví, Andrés Gil-Imaz
Publikováno v:
Springer Geology ISBN: 9783031166921
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57bceb24717778367208aea08dd016b3
https://doi.org/10.1007/978-3-031-16693-8_5
https://doi.org/10.1007/978-3-031-16693-8_5
Autor:
Antonio M. Casas-Sainz, Pablo Santolaria, Tania Mochales, Andrés Pocoví, Esther Izquierdo, Hmidou El-Ouardi, Bennacer Moussaid, Ahmed Manar, Vicente C. Ruiz-Martínez, Marcos Marcén, Sara Torres-López, Andrés Gil-Imaz, Teresa Román-Berdiel, Belén Oliva-Urcia, Pablo Calvín
Publikováno v:
Springer Geology ISBN: 9783031166921
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f3e5f17b40bcccd914aafbd13a2ec477
https://doi.org/10.1007/978-3-031-16693-8_2
https://doi.org/10.1007/978-3-031-16693-8_2
Autor:
Daniel Vizcaïno, Eric Monceret, J. Javier Álvaro, Andrés Gil Imaz, André Pouclet, Jacques-Marie Bardintzeff
Publikováno v:
Geoscience Frontiers, Vol 8, Iss 1, Pp 25-64 (2017)
Geoscience Frontiers
Geoscience Frontiers, Elsevier, 2017, 8, pp.25-64. ⟨10.1016/j.gsf.2016.03.002⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Geoscience Frontiers
Geoscience Frontiers, Elsevier, 2017, 8, pp.25-64. ⟨10.1016/j.gsf.2016.03.002⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
The Cambrian–lower Ordovician volcanic units of the South Armorican and Occitan domains are analysed in a tectonostratigraphic survey of the French Variscan Belt. The South Armorican lavas consist of continental tholeiites in middle Cambrian–Furo
Publikováno v:
Studia Geophysica et Geodaetica. 57:692-709
We analyse paramagnetic, ferrimagnetic and frequency-dependent susceptibility in the southern Pyrenees and northern Ebro basin. The analyzed rocks show a wide range of values for the three parameters within the different lithological groups. Sandston
Autor:
Antonio M. Casas-Sainz, Emilio L. Pueyo, Andrés Pocoví Juan, Óscar Pueyo Anchuela, Andrés Gil Imaz
Publikováno v:
Terra Nova. 25:307-314
Magnetic susceptibility in rocks is the sum of the contributions of different magnetic particles (paramagnetic, diamagnetic and ferromagnetic s.l.). These contributions can be measured at variable temperatures or at variable fields (hysteresis loops)
Publikováno v:
International Journal of Earth Sciences. 102:1131-1149
A combined sedimentological, shape-preferred orientation and anisotropy of magnetic susceptibility (AMS) analysis has been performed at the Arroyofrio Bed (Callovian–Oxfordian boundary level) in the locality of Moneva (Iberian Range, NE Spain). The
Publikováno v:
Comptes Rendus Geoscience. 343:11-19
Fine-grained sediments are generally better strain-markers in the outer part of orogenic belts and foreland basins because they are more prone to cleavage formation than coarse detrital rocks in diagenetic to very-low metamorphic environments. This a
Publikováno v:
Tectonophysics. 461:215-227
This paper presents a multidisciplinary approach (stratigraphic, sedimentologic, structural, and mineralogic) to document the evidences for Cadomian and earliest-Cambrian tectonic processes recorded in the Iberian Chains, which were strongly overprin