Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Gisella Palma"'
Autor:
Diana Comte, Gisella Palma, Jimena Vargas, Daniela Calle-Gardella, Matías Peña, Sergio García-Fierro, Joëlle D’Andres, Steven Roecker, Sergio Pichott
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-13 (2023)
Abstract An essential part of the world's remaining mineral resources is expected to reside deep in the crust or under post-mineralization cover. For porphyry copper deposits, the world’s primary source of Cu, Mo, and Re, identifying the dynamic pr
Externí odkaz:
https://doaj.org/article/e875f3ac0b314aadac08a2b6a9332a30
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Abstract Magnetite is the main constituent of iron oxide–apatite (IOA) deposits, which are a globally important source of Fe and other elements such as P and REE, critical for modern technologies. Geochemical studies of magnetite from IOA deposits
Externí odkaz:
https://doaj.org/article/f21bd5a023004768a8f7859f6aa32edd
Publikováno v:
Mineralium Deposita. 58:379-402
Autor:
J. Tomás Ovalle, Martin Reich, Fernando Barra, Adam C. Simon, Artur P. Deditius, Margaux Le Vaillant, Owen K. Neill, Gisella Palma, Rurik Romero, Nelson Román, Nikita L. La Cruz, Malcolm P. Roberts, Diego Morata
Publikováno v:
Geochimica et Cosmochimica Acta. 330:230-257
Autor:
J. Tomás Ovalle, Martin Reich, Fernando Barra, Adam C. Simon, Belinda Godel, Margaux Le Vaillant, Gisella Palma, Artur P. Deditius, Gert Heuser, Gloria Arancibia, Diego Morata
Publikováno v:
ACS Earth and Space Chemistry.
Publikováno v:
Scientific Reports
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Magnetite is the main constituent of iron oxide–apatite (IOA) deposits, which are a globally important source of Fe and other elements such as P and REE, critical for modern technologies. Geochemical studies of magnetite from IOA deposits have prov
Autor:
Gisella Palma, Fernando Barra, Rurik Romero, Jeffrey D. Vervoort, Martin Reich, Adam C. Simon, Mathieu Leisen, Victor A. Valencia
Publikováno v:
Geochimica et Cosmochimica Acta. 246:515-540
The ratio of the halogens F and Cl in apatite is highly sensitive to changes in the composition of an evolving silicate melt or aqueous fluid. For this reason apatite chemistry is widely used as a monitor of halogen behavior in magmatic-hydrothermal
Publikováno v:
Goldschmidt2021 abstracts.
Publikováno v:
Ore Geology Reviews. 126:103748
Magnetite is the most important iron ore in iron oxide-apatite (IOA) deposits which represent the Cu-poor end-member of the iron oxide-copper–gold (IOCG) clan. Magnetite chemistry has been used as a petrogenetic indicator to identify the geological
Autor:
Fernando Barra, Martin Reich, Eduardo Salazar, David Selby, Adam C. Simon, Gisella Palma, Paula A Rojas
Publikováno v:
Ore geology reviews, 2017, Vol.81(Part 1), pp.62-78 [Peer Reviewed Journal]
Ore Geology Reviews
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Ore Geology Reviews
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The Andean IOCG clan in the Coastal Cordillera of northern Chile, comprises the iron oxide-Cu-Au sensu stricto, the iron oxide-apatite (IOA), and the stratabound Cu(− Ag) deposits, also known as Manto-type Cu(− Ag) deposits. IOCGs and Manto-type
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::49c13b5e4b153fc30306203dce486aee
http://dro.dur.ac.uk/20115/
http://dro.dur.ac.uk/20115/