Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Pérez Ramos, Isaac"'
Autor:
Barberá Fornell, Juan Antonio, Mudarra Martínez, Matías, Marín Guerrero, Ana Isabel, Andreo Navarro, Bartolomé, Vadillo Pérez, Iñaki, Neukum, Christoph, Sánchez García, Damián, Pérez Ramos, Isaac, Ortega Rodríguez, Luis
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
La realización de un ensayo multitrazador en la cabecera del río Turón (Serranía de Ronda oriental, Málaga) ha permitido definir las áreas de recarga y descarga, así como precisar el funcionamiento hidrogeológico de los acuíferos carbonátic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::5b331a869b1f879ed423373427ab24ce
https://hdl.handle.net/10272/7220
https://hdl.handle.net/10272/7220
Autor:
Mudarra Martínez, Matías, Marín Guerrero, Ana Isabel, Andreo Navarro, Bartolomé, Vadillo Pérez, Iñaki, Barberá Fornell, Juan Antonio, Neukum, Christoph, Sánchez García, Damián, Liñán Baena, Cristina, Pérez Ramos, Isaac
A multi-tracer test was done in the Alta Cadena and Los Tajos mountains range (Malaga province, southern Spain) in order to delimitate the aquifer system drained by Villanueva del Rosario spring and to precise its hydrogeological behaviour. The resul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::8ccd6503860369991db7e5ddf498b128
Autor:
Mudarra Martínez, Matías, Marín Guerrero, Ana Isabel, Andreo Navarro, Bartolomé, Vadillo Pérez, Iñaki, Barberá Fornell, Juan Antonio, Neukum, Christoph, Sánchez García, Damián, Liñán Baena, Cristina, Pérez Ramos, Isaac
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
A multi-tracer test was done in the Alta Cadena and Los Tajos mountains range (Malaga province, southern Spain) in order to delimitate the aquifer system drained by Villanueva del Rosario spring and to precise its hydrogeological behaviour. The resul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::8ccd6503860369991db7e5ddf498b128
http://hdl.handle.net/10272/7891
http://hdl.handle.net/10272/7891
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
In Montalvo beach (Pontevedra) a concentration of heavy minerals forming a placer takes place. The placer formation is related to the beach hydrodynamics that concentrates and segregates the different particles in layers. It is located in the north z
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::7bd62a5ef313ab4771686960017aecc1
http://hdl.handle.net/10272/8264
http://hdl.handle.net/10272/8264
In Montalvo beach (Pontevedra) a concentration of heavy minerals forming a placer takes place. The placer formation is related to the beach hydrodynamics that concentrates and segregates the different particles in layers. It is located in the north z
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::7bd62a5ef313ab4771686960017aecc1
https://hdl.handle.net/10272/8264
https://hdl.handle.net/10272/8264
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
Arias Montano. Repositorio Institucional de la Universidad de Huelva
4 páginas, 3 figuras.-- Trabajo presentado en la 37ª Sesión Científica, Almería, 2004.
By means of a photointerpretation study, the main fault sets have been determined in the Sierra Almijara, in the Betic Cordillera. The more frequent dire
By means of a photointerpretation study, the main fault sets have been determined in the Sierra Almijara, in the Betic Cordillera. The more frequent dire
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::94dfd888bf2e005d96a67b51b378df58
http://hdl.handle.net/10261/29378
http://hdl.handle.net/10261/29378
By means of a photointerpretation study, the main fault sets have been determined in the Sierra Almijara, in the Betic Cordillera. The more frequent directions are N20-40E, N50-70E, N90-100E, N120-140E and N140-160E. They are consistent with some of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::94dfd888bf2e005d96a67b51b378df58
https://hdl.handle.net/10272/8805
https://hdl.handle.net/10272/8805
Autor:
Andreo Navarro, Bartolomé, Vadillo Pérez, Iñaki, Carrasco Cantos, Francisco, Neukum, Christoph, Jiménez Gavilán, Pablo, Liñán Baena, Cristina, Goldscheider, Nico, Hötzl, H., Ferrer, R., Campo, L. del, Göppert, N., Vías, J. M., Pérez Ramos, Isaac, Sánchez García, Damián, Cobos, Alberto
A tracer test during low-flow conditions was carried out in the karstic aquifer of Sierra de las Nieves (Málaga) in order to assess its hydrogeological functioning and vulnerability to contamination. Two kilogrammes of Eosine were injected in an act
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::a00141633cc72022e54f9765c0ea3dc5
https://hdl.handle.net/10272/8829
https://hdl.handle.net/10272/8829
The Río de la Miel fault shows a complex movement history. Three main displacement stages have been distinguished from the microtectonic analysis. The first stage was a dextral strike-slip movement whose cr, was almost horizontal with, a NNW-SSE dir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::353569a1ef799b82f3fc6140262a48b6
https://hdl.handle.net/10272/8953
https://hdl.handle.net/10272/8953
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Río de la Miel fault shows a complex movement history. Three main displacement stages have been distinguished from the microtectonic analysis. The first stage was a dextral strike-slip movement whose cr, was almost horizontal with, a NNW-SSE dir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::353569a1ef799b82f3fc6140262a48b6
http://hdl.handle.net/10272/8953
http://hdl.handle.net/10272/8953