Wyatt M. Bain
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View article: Magnetite-apatite ores record widespread involvement of molten salts
Magnetite-apatite ores record widespread involvement of molten salts Open
The origins of magnetite-apatite deposits are controversial, and the crux of the debate is what types of fluids form these rocks. We present evidence from 20 magnetite-apatite deposits worldwide showing ubiquitous involvement of molten sal…
View article: Correction to: The geology, geochemistry, and magmatic evolution of the Legris Lake mafic–ultramafic complex, Ontario, Canada
Correction to: The geology, geochemistry, and magmatic evolution of the Legris Lake mafic–ultramafic complex, Ontario, Canada Open
View article: Magmatic immiscibility and the origin of magnetite-(apatite) iron deposits
Magmatic immiscibility and the origin of magnetite-(apatite) iron deposits Open
View article: The geology, geochemistry, and magmatic evolution of the Legris Lake mafic–ultramafic complex, Ontario, Canada
The geology, geochemistry, and magmatic evolution of the Legris Lake mafic–ultramafic complex, Ontario, Canada Open
The Archean Legris Lake mafic–ultramafic complex (LLC) is spatially (~ 12 km east) and temporally (2690.59 ± 0.77 Ma) associated with the world-class Lac des Iles (LDI) palladium deposit. Modeling of whole-rock major-element compositions s…
View article: Vein-type gold formation during late extensional collapse of the Eastern Desert, Egypt: the Gidami deposit
Vein-type gold formation during late extensional collapse of the Eastern Desert, Egypt: the Gidami deposit Open
Orogenic gold deposits, though construed to focused fluid flow during orogenesis, commonly post-date the main accretionary events. Several lines of evidence indicate that orogenic gold formation in the Arabian–Nubian Shield continued throu…
View article: Magmatic immiscibility and the origin of magnetite-(apatite) iron deposits
Magmatic immiscibility and the origin of magnetite-(apatite) iron deposits Open
The origin of magnetite-(apatite) iron deposits (MtAp) is among the most contentious issue in ore geology with competing models involving purely hydrothermal to magmatic processes. We study here melt inclusions trapped in plagioclase pheno…
View article: The Geology, Geochemistry, and Magmatic Evolution of the Legris Lake Mafic-Ultramafic Complex.
The Geology, Geochemistry, and Magmatic Evolution of the Legris Lake Mafic-Ultramafic Complex. Open
View article: Evidence for iron-rich sulfate melt during magnetite(-apatite) mineralization at El Laco, Chile
Evidence for iron-rich sulfate melt during magnetite(-apatite) mineralization at El Laco, Chile Open
The origins of Kiruna-type magnetite(-apatite) [Mt(-Ap)] deposits are contentious, with existing models ranging from purely hydrothermal to orthomagmatic end members. Here, we evaluate the compositions of fluids that formed the classic yet…
View article: Supplemental Material: Evidence for iron-rich sulfate melt during magnetite(-apatite) mineralization at El Laco, Chile
Supplemental Material: Evidence for iron-rich sulfate melt during magnetite(-apatite) mineralization at El Laco, Chile Open
Additional details on the geologic setting, analytical methods and results, Figures S1–S6, and Tables S1 and S2.
View article: Supplemental Material: Evidence for iron-rich sulfate melt during magnetite(-apatite) mineralization at El Laco, Chile
Supplemental Material: Evidence for iron-rich sulfate melt during magnetite(-apatite) mineralization at El Laco, Chile Open
Additional details on the geologic setting, analytical methods and results, Figures S1–S6, and Tables S1 and S2.
View article: Testing Established Models of Hydrothermal Fluid Distribution Around Porphyry Deposits: The Application of Fluid Inclusion Research to Porphyry Deposit Exploration
Testing Established Models of Hydrothermal Fluid Distribution Around Porphyry Deposits: The Application of Fluid Inclusion Research to Porphyry Deposit Exploration Open
The Kabba porphyry copper prospect in northwestern Arizona contains two zones of porphyry style mineralization and alteration, which are spatially separated by a north-south trending normal fault. These two zones are referred to as the Kab…
View article: Extreme fractionation and magmatic–hydrothermal transition in the formation of the Abu Dabbab rare-metal granite, Eastern Desert, Egypt
Extreme fractionation and magmatic–hydrothermal transition in the formation of the Abu Dabbab rare-metal granite, Eastern Desert, Egypt Open
Funder: \n http://dx.doi.org/10.13039/501100003753\n MacEwan University