Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Darío Chinchilla"'
Autor:
Javier Escuder-Viruete, Eduardo A. Molina, Darío Chinchilla, Janet Gabites, Raúl Seggiaro, Cintia A. Marquetti, Nemesio Heredia
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
Convenio SEGEMAR - CN IGMECSIC
In the Cenozoic Central Volcanic Zone of the Andes, the genetic relationships between regional deformation, volcanic activity, and epithermal mineralization are not fully established. In order to shed some light on
In the Cenozoic Central Volcanic Zone of the Andes, the genetic relationships between regional deformation, volcanic activity, and epithermal mineralization are not fully established. In order to shed some light on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::91e8462833e14984899cd734493c242b
https://doi.org/10.1016/j.jsg.2022.104582
https://doi.org/10.1016/j.jsg.2022.104582
Autor:
Darío Chinchilla, Fernando Nieto, Rosario Lunar, Raúl Merinero, Rubén Piña, Xabier Arroyo, Lorena Ortega
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
Two textural types of chlorite are identified in the mineralised veins at the Patricia Zn-Pb-Ag epithermal ore deposit (NE, Chile): massive and oscillatory-zoned radiated chlorites. Three main stages of mineralisation have been defined in the Patrici
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ee762b924e242921824b91618f89a33c
http://hdl.handle.net/10261/184238
http://hdl.handle.net/10261/184238
Autor:
Cecilio Quesada, Lorena Ortega, Robert J. Bodnar, Rosario Lunar, Raúl Merinero, D. Moncada, Rubén Piña, Darío Chinchilla, Antonio Valverde
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
Ore Geology Reviews
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
instname
Ore Geology Reviews
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The Patricia ore deposit represents an unusual example of economic Zn–Pb–Ag mineralization at the northernmost end of the Late Eocene–Oligocene metallogenic belt in Chile. It is hosted by volcano-sedimentary units, which are typically tuffaceou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d62a8e33dcf231dfbd788962cc30a732
http://hdl.handle.net/10261/125335
http://hdl.handle.net/10261/125335