Zobrazeno 1 - 10
of 100
pro vyhledávání: '"Torcal, F."'
Publikováno v:
In Tectonophysics 9 July 2024 882
Publikováno v:
In Journal of Volcanology and Geothermal Research September 2023 441
Autor:
González Pacheco, N., Marañón Pardillo, R., Storch de Gracia Calvo, P., Campos Calleja, C., Mojica Muñoz, E., Rodríguez Sáez, M.J., Crespo Rupérez, E., Panzino Occhiuzzo, F., Díez Sáez, C., Barea Martínez-Páis, V., Hernández González, A., Estopiñá Ferrer, G., Yagüe Torcal, F., Pociello Almiñana, N., García Peleteiro, P., Pizà Oliveras, A.
Publikováno v:
In Anales de Pediatria April 2014 80(4):242-248
Autor:
Azañón, José Miguel, Azor, A., Booth Rea, G., Martín Rosales, Wenceslao, Justo Alpaflés, J. L. de, Torcal, F., Torcal, M.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Alhambra is built on a conglomeratic formation, known as the Alhambra Formation, whose age is Pliocene to Lower Pleistocene and has a visible thickness of 200 metres. The western part of the San Pedro escarpment corresponds to a fault-scarp with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::50a2d4e83e2b5fd2e4451454aee23dd6
http://hdl.handle.net/10272/9059
http://hdl.handle.net/10272/9059
Autor:
Azañón, José Miguel, Azor, A., Booth Rea, G., Martín Rosales, Wenceslao, Justo Alpaflés, J. L. de, Torcal, F., Torcal, M.
The Alhambra is built on a conglomeratic formation, known as the Alhambra Formation, whose age is Pliocene to Lower Pleistocene and has a visible thickness of 200 metres. The western part of the San Pedro escarpment corresponds to a fault-scarp with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::50a2d4e83e2b5fd2e4451454aee23dd6
Autor:
Azanon, J.M., Azor, A., Booth-Rea, G., Martín-Rosales, W., de Justo-Alpañes, J.L., Torcal, F., Espinar, M.
Publikováno v:
Geogaceta, 34 . pp. 159-162.
The Alhambra is built on a conglomeratic formation, known as the Alhambra Formation, whose age is Pliocene to Lower Pleistocene and has a visible thickness of 200 metres. The western part of the San Pedro escarpment corresponds to a fault-scarp with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2386::3c4b97cbf53a3be3287d5aae19119411
http://oceanrep.geomar.de/7283/
http://oceanrep.geomar.de/7283/
Akademický článek
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Autor:
Galindo Zaldívar, Jesús, Jabaloy, A., Serrano, I., Morales, J., González Lodeiro, Francisco, Torcal, F.
The analysis of the seismic activity and the microtectonic study of outcrops located in the southeastern Granada Depression show that the stress states have been heterogeneous from the Upper Miocene up to the present. NE-SW extensional stresses may b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::71a67c265a43043a7928e7079ca59aa2
Autor:
Galindo Zaldívar, Jesús, Jabaloy, A., Serrano, I., Morales, J., González Lodeiro, Francisco, Torcal, F.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The analysis of the seismic activity and the microtectonic study of outcrops located in the southeastern Granada Depression show that the stress states have been heterogeneous from the Upper Miocene up to the present. NE-SW extensional stresses may b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::71a67c265a43043a7928e7079ca59aa2
http://hdl.handle.net/10272/10303
http://hdl.handle.net/10272/10303
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
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K zobrazení výsledku je třeba se přihlásit.