Now showing items 1-8 of 8

    • Rodríguez Mustafa, María A.; Simon, Adam C.; Real Contreras, Irene del; Thompson, John F.H.; Bilenker, Laura D.; Barra Pantoja, Fernando; Bindeman, Ilya (Society of Economic Geologists (SEG), 2020)
      Iron oxide copper-gold (IOCG) and iron oxide-apatite (IOA) deposits are major sources of Fe, Cu, and Au. Magnetite is the modally dominant and commodity mineral in IOA deposits, whereas magnetite and hematite are predominant ...
    • González Jiménez, José; Barra Pantoja, Fernando; Garrido, Leonardo; Reich Morales, Martín; Satsukawa, Takako; Romero, Rurik; Salazar, Eduardo; Colás, Vanessa; Orellana, Felipe; Rabbia, Osvaldo; Plissart, Gaëlle; Morata Céspedes, Diego (Elsevier, 2016)
      Platinum-group element (PGE) and gold inclusions are usually present in peridotites and chromitite deposits associated with ophiolites. Here, we present the first detailed study of the mineralogy of precious metals in ...
    • Childress, Tristan M.; Simon, Adam C.; Reich Morales, Martín; Barra Pantoja, Fernando; Arce, Mauricio; Lundstrom, Craig C.; Bindeman, Ilya N. (Springer, 2020)
      The Mantoverde iron oxide-copper-gold (IOCG) deposit, Chile, contains hundreds of millions of tonnes (Mt) of mineable iron oxide and copper sulfide ore. While there is an agreement that mineralization at Mantoverde was ...
    • La Cruz, Nikita L.; Ovalle, J. Tomás; Simon, Adam C.; Konecke, Brian A.; Barra Pantoja, Fernando; Reich Morales, Martín; Leisen, Mathieu; Childress, Tristan M. (Society of Economic Geologists, USA, 2020)
      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 ...
    • González Jiménez, José; Plissart, Gaelle; Garrido, Leonardo; Padron Navarta, José; Aiglsperger, Thomas; Romero, Rurik; Marchesi, Claudio; Moreno Abril, Antonio; Reich Morales, Martín; Barra Pantoja, Fernando; Morata Céspedes, Diego (E Schweizerbartsche Verlagsbuchhandlung, 2017)
      Humite minerals, including Ti-rich, hydroxyl-dominant chondrodite and clinohumite, occur in Paleozoic antigorite serpentinite in the La Cabana area, in the Chilean Coastal Cordillera (similar to 38 degrees 30'S- 73 degrees ...
    • Childress, Tristán; Simon, Adam C.; Reich Morales, Martín; Barra Pantoja, Fernando; Bilenker, Laura D.; La Cruz, Nikita L.; Bindeman, Ilya N.; Ovalle Ortega, José (Society of Economic Geologists, USA, 2020)
      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 ...
    • Tassara, Santiago; Reich Morales, Martín; Konecke, Brian A.; González Jiménez, José María; Simon, Adam C.; Morata Céspedes, Diego; Barra Pantoja, Fernando; Fiege, Adrián; Schilling, Manuel E.; Corgne, Alexandre (Frontiers Media, 2020)
      The oxidation state of the Earth's mantle and its partial melting products exert a key control on the behavior and distribution of sulfur and chalcophile and siderophile elements between the mantle and crust, underpinning ...
    • Barra Pantoja, Fernando; Reich Morales, Martín; Selby, David; Rojas, Paula; Simon, Adam C.; Salazar, Eduardo; Palma, Gisella (Elsevier, 2017)
      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) ...