Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Millán Garrido, H."'
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Based on structural, stratigraphic and gravimetric data, a regional scale N 020-040 E blind-fault, named the Oroz-Betelu- Unzue fault, extending from the western part of the Oroz-Betelu massif to the Sierra de Alaiz thrust front, is inferred. This fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::b1bc4d88f9014e23d919e405ba1301ce
http://hdl.handle.net/10272/8436
http://hdl.handle.net/10272/8436
Based on structural, stratigraphic and gravimetric data, a regional scale N 020-040 E blind-fault, named the Oroz-Betelu- Unzue fault, extending from the western part of the Oroz-Betelu massif to the Sierra de Alaiz thrust front, is inferred. This fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::b1bc4d88f9014e23d919e405ba1301ce
https://hdl.handle.net/10272/8436
https://hdl.handle.net/10272/8436
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The structure of the eastern extreme of the Jaca Basin is defined by the Gavarnie, Guara-Gèdre and Guarga thrust sheets. The Guara-Gèdre thrust was active during mid Luttetian-earliest Chattian and the Gavarnie thrust, that results from the inversi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::0d286c34fabb06d8ffe7048a923ff4c5
http://hdl.handle.net/10272/8579
http://hdl.handle.net/10272/8579
Autor:
Gil Imaz, Andrés, Simón Gómez, José Luis, Pueyo Anchuela, Óscar, Millán Garrido, H., Pocoví Juan, Andrés, Andrés, José Antonio, Arantegui, A., Arlegui, L. E., Arranz, Enrique, Liesa, Carlos L., Artieda, O., Corella, Juan Pablo, Edo Romero, Vanesa, Galindo, Gloria, Maestro González, Adolfo, Sánchez, E., Rico, M. T., Simón, M., Tyrrell, J.
Geometric and kinematic analysis of Pyrenean folds, cleavage and thrusts is carried out in several exceptional outcrops of the Eocene flysch at Isaba (Navarra, Spain). Distribution, orientation and cross-cut relationships between these structures sug
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::cf6da48963fba1488961362ae6133d1b
https://hdl.handle.net/10272/8564
https://hdl.handle.net/10272/8564
Autor:
Gil Imaz, Andrés, Simón Gómez, José Luis, Pueyo Anchuela, Óscar, Millán Garrido, H., Pocoví Juan, Andrés, Andrés, José Antonio, Arantegui, A., Arlegui, L. E., Arranz, Enrique, Liesa, Carlos L., Artieda, O., Corella, Juan Pablo, Edo Romero, Vanesa, Galindo, Gloria, Maestro González, Adolfo, Sánchez, E., Rico, M. T., Simón, M., Tyrrell, J.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Geometric and kinematic analysis of Pyrenean folds, cleavage and thrusts is carried out in several exceptional outcrops of the Eocene flysch at Isaba (Navarra, Spain). Distribution, orientation and cross-cut relationships between these structures sug
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::cf6da48963fba1488961362ae6133d1b
http://hdl.handle.net/10272/8564
http://hdl.handle.net/10272/8564
The structure of the eastern extreme of the Jaca Basin is defined by the Gavarnie, Guara-Gèdre and Guarga thrust sheets. The Guara-Gèdre thrust was active during mid Luttetian-earliest Chattian and the Gavarnie thrust, that results from the inversi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::0d286c34fabb06d8ffe7048a923ff4c5
https://hdl.handle.net/10272/8579
https://hdl.handle.net/10272/8579
Publikováno v:
Acta Geologica Hispanica; Vol.: 32 Núm.: 3-4; 237-256
RCUB. Revistas Científicas de la Universidad de Barcelona
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Acta geológica hispánica; 1997: Vol.: 32 Núm.: 3-4; p. 237-256
RCUB. Revistas Científicas de la Universidad de Barcelona
instname
Acta geológica hispánica; 1997: Vol.: 32 Núm.: 3-4; p. 237-256
The magnetotectonic analysis of 32 sites located along the External Sierras (mainly in Middle Eocene marls) shows the primary character of the magnetisation and pennits the differences between the paleovectors obtained to be interpreted as a result o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::f987cfeee636a3d648a304de754764fc
https://revistes.ub.edu/index.php/ActaGeologica/article/view/4613
https://revistes.ub.edu/index.php/ActaGeologica/article/view/4613
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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[ES] El estudio magnetotectónico de 32 estaciones localizadas, principalmente, en las margas de la formación Arguis a lo largo de las Sierras Exteriores Aragonesas (Pirineo Suroccidental) nos ha permitido caracterizar la estabilidad y el carácter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ddcd06531fc5980a26c97eb5fa46d756
http://hdl.handle.net/10261/6741
http://hdl.handle.net/10261/6741
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
In the western part of the Sierras Exteriores Aragonesas the southern Pyrenean front is not a southvergent large thrust, but an isoclinal detachment fold (Santo Domingo anticline), whose core is occuppied by the Upper Triassic (Keuper facies). Twenty
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::379244724425237324a3bb900ff8bb5f
http://hdl.handle.net/10272/12473
http://hdl.handle.net/10272/12473
Autor:
Larrasoaña, J. C., Pueyo Morer, Emilio L., Valle de Lersundi, J. del, Millán Garrido, H., Parés, J. M., Pocoví Juan, Andrés, Dinarès Turell, Jaume
This paper presents the first magnetotectonic data of the central fringe of the Jaca-Pamplona Basin. These data have been obtained from 16 sites located in marls, tirbidites and limestones of Eocene age. In the central and Eastern sectors of the basi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::d8bb5f3f04ea72fbd85489b5969eb699