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Episodic hydrothermal alterations in the Sierra de Guadarrama took place between ca. 300 Ma and 10 Ma. New K-Ar ages for hydrothermal minerals have been obtained that along with previous data allow to better constrain the late- to post-Variscan histo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::3cc326cb098037b128b4207ca690debf
https://hdl.handle.net/10272/17899
https://hdl.handle.net/10272/17899
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
Episodic hydrothermal alterations in the Sierra de Guadarrama took place between ca. 300 Ma and 10 Ma. New K-Ar ages for hydrothermal minerals have been obtained that along with previous data allow to better constrain the late- to post-Variscan histo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1d709808b13c464493fb6748b00e1d03
http://hdl.handle.net/10272/17899
http://hdl.handle.net/10272/17899