Wernecke breccia, Canada: A large-scale Proterozoic IOCG system related to basin evolution

[1]  D. Thorkelson,et al.  Regional-scale Proterozoic IOCG-mineralized breccia systems: examples from the Wernecke Mountains, Yukon, Canada , 2005 .

[2]  J. Hunt.  The geology and genesis of iron oxide-copper-gold mineralisation associated with Wernecke Breccia, Yukon, Canada , 2005 .

[3]  R. Creaser,et al.  Early Mesoproterozoic intrusive breccias in Yukon, Canada: the role of hydrothermal systems in reconstructions of North America and Australia , 2001 .

[4]  R. Creaser,et al.  Early Proterozoic magmatism in Yukon, Canada: constraints on the evolution of northwestern Laurentia , 2001 .

[5]  P. Pollard.  Sodic(–calcic) alteration in Fe-oxide–Cu–Au districts: an origin via unmixing of magmatic H2O–CO2–NaCl ± CaCl2–KCl fluids , 2001 .

[6]  David A. Johnson.  ALTERNATIVE BRINE SOURCES FOR Fe-OXIDE(-Cu-Au) SYSTEMS: IMPLICATIONS FOR HYDROTHERMAL ALTERATION AND METALS , 2000 .

[7]  M. Barton,et al.  Evaporitic-source model for igneous-related Fe oxide-(REE-Cu-Au-U) mineralization , 1996 .

[8]  N. Oreskes,et al.  Geological characteristics and tectonic setting of proterozoic iron oxide (CuUAuREE) deposits , 1992 .

[9]  R. A. Lane.  Geologic setting and petrology of the Proterozoic Ogilvie Mountains breccia of the Coal Creek inlier, southern Ogilvie Mountains, Yukon Territory , 1990 .

[10]  R. T. Bell.  Megabreccias in northeastern Wernecke Mountains, Yukon Territory , 1986 .

[11]  G. Delaney.  The Middle Proterozoic Wernecke Supergroup, Wernecke Mountains, Yukon Territory , 1981 .