Zobrazeno 1 - 10
of 50
pro vyhledávání: '"González Casado, J. M."'
Autor:
González Casado, J. M., Giner Robles, J. L., Gumiel Martínez, Pablo, García Cuevas, C., Moreno, A.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Pleistocene;karst¡c deposits developed into Upper Cretaceous limestones of the Prebetic zone, in the . boundary region between the Iberian and Betic chains, were sampled in order to investigate the calcite e-tyyin.occurrence in these modern sediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::1682e4f4b3ef76c0b93d5a737b5c1645
http://hdl.handle.net/10272/8925
http://hdl.handle.net/10272/8925
Autor:
González Casado, J. M., Giner Robles, J. L., Gumiel Martínez, Pablo, García Cuevas, C., Moreno, A.
Pleistocene;karst¡c deposits developed into Upper Cretaceous limestones of the Prebetic zone, in the . boundary region between the Iberian and Betic chains, were sampled in order to investigate the calcite e-tyyin.occurrence in these modern sediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::1682e4f4b3ef76c0b93d5a737b5c1645
https://hdl.handle.net/10272/8925
https://hdl.handle.net/10272/8925
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Spanish Central System (SCS) is an intraplate mountain range located in the central part of the Iberian Peninsula, and consists, for the most part, of piutonic and metamorphic rocks belonging to the Hercynian basement and a locally preserved thin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::531518bb87e0fde198db5137098924ef
http://hdl.handle.net/10272/9316
http://hdl.handle.net/10272/9316
The Spanish Central System (SCS) is an intraplate mountain range located in the central part of the Iberian Peninsula, and consists, for the most part, of piutonic and metamorphic rocks belonging to the Hercynian basement and a locally preserved thin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::531518bb87e0fde198db5137098924ef
A detailed geological map of 118 fault traces that form the Rio Maro Fault Zone (Malaga, Spain) has been carried out, emphasizing their geometric and kinematics characteristics. Several fault population analysis methods have been applied among them t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::a8a7ae0138c4f8e412eecb8514c90e16
https://hdl.handle.net/10272/9404
https://hdl.handle.net/10272/9404
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
A detailed geological map of 118 fault traces that form the Rio Maro Fault Zone (Malaga, Spain) has been carried out, emphasizing their geometric and kinematics characteristics. Several fault population analysis methods have been applied among them t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::a8a7ae0138c4f8e412eecb8514c90e16
http://hdl.handle.net/10272/9404
http://hdl.handle.net/10272/9404
El análisis de las trazas de fisión en apatitos procedentes de los metasedimentos de bajo grado metamòrfico de la Formación Miers Bluff (Península Hurd, Isla Livingston, Islas Shetland del Sur) muestra que el enfriamiento posterior al pico metam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::fea396f1577c6bc525ace2b41c26297b
https://hdl.handle.net/10272/9840
https://hdl.handle.net/10272/9840
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
El análisis de las trazas de fisión en apatitos procedentes de los metasedimentos de bajo grado metamòrfico de la Formación Miers Bluff (Península Hurd, Isla Livingston, Islas Shetland del Sur) muestra que el enfriamiento posterior al pico metam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::fea396f1577c6bc525ace2b41c26297b
http://hdl.handle.net/10272/9840
http://hdl.handle.net/10272/9840
Autor:
Muñoz Martín, Alfonso, Giner Robles, J. L., González Casado, J. M., López Martínez, Jerónimo, Durán Valsero, Juan José, Gumiel Martínez, Pablo, Serrano, E.
The geophysical study of superficial deposits (mainly gravels) in ice-free areas near the seashore in the South Shetland Islands (Antarctica) allows establishing the possible existence of permafrost and buried ice bodies. In this work we have investi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::9d6679318531697e57ba29d82390c4e5
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The statistical study of the post-hercynian cartographic faults of the Northwest part of Spain (Galicia) allow to precise the existence of three main fault sets; NE-SW, NW-SE and N-S, which controlled the topograpic features in this area. The seismic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::d999840ef5c0884c60ee2f69016cf1fd
http://hdl.handle.net/10272/9897
http://hdl.handle.net/10272/9897