Zobrazeno 1 - 7
of 7
pro vyhledávání: '"J. Tomás Ovalle"'
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
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.
Autor:
Mathieu Leisen, Martin Reich, Fernando Barra, Tristan M. Childress, J. Tomás Ovalle, Nikita L. La Cruz, Brian A. Konecke, Adam C. Simon
Publikováno v:
Economic Geology. 115:1461-1491
The textures of outcrop and near-surface exposures of the massive magnetite orebodies (>90 vol % magnetite) at the Plio-Pleistocene El Laco iron oxide-apatite (IOA) deposit in northern Chile are similar to basaltic lava flows and have compositions th
Autor:
Tristan M. Childress, Laura D. Bilenker, Adam C. Simon, Fernando Barra, Nikita L. La Cruz, Martin Reich, J. Tomás Ovalle, Ilya N. Bindeman
Publikováno v:
Economic Geology. 115:1519-1536
The Plio-Pleistocene El Laco iron oxide-apatite (IOA) orebodies in northern Chile are some of the most enigmatic mineral deposits on Earth, interpreted to have formed as lava flows or by hydrothermal replacement, two radically different processes. Fi
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:
J. Tomás Ovalle, Maria A. Rodriguez-Mustafa, Artur P. Deditius, Martin Reich, Adam C. Simon, Diego Morata, Tristan M. Childress, Fernando Barra, Brian A. Konecke, Nikita L. La Cruz
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-11 (2018)
Scientific Reports
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Scientific Reports
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The genetic link between magmas and ore deposit formation is well documented by studies of fossil hydrothermal systems associated with magmatic intrusions at depth. However, the role of explosive volcanic processes as active agents of mineralization