N. Rosengren

发表

Were intercalated komatiites and dacites at the Black Swan nickel sulphide mine, Yilgarn Craton, Western Australia, emplaced as extrusive lavas or intrusive bodies? The significance of breccia textures and contact relationships

R. Cas, Katherine Marks, J. Trofimovs, 2013 .

Contrasting komatiite belts, associated Ni–Cu–(PGE) deposit styles and assimilation histories

T. McCuaig, S. Beresford, M. Fiorentini, 2010 .

Controls on the emplacement and genesis of the MKD5 and Sarah’s Find Ni–Cu–PGE deposits, Mount Keith, Agnew–Wiluna Greenstone Belt, Western Australia

S. Beresford, M. Fiorentini, M. Barley, 2007 .

Reconstruction of an extensive Archaean dacitic submarine volcanic complex associated with the komatiite-hosted Mt Keith nickel deposit, Agnew-Wiluna Greenstone Belt, Yilgarn Craton, Western Australia

R. Cas, S. Beresford, N. Rosengren, 2008 .

District to Camp Controls on the Genesis of Komatiite-Hosted Nickel Sulfide Deposits, Agnew-Wiluna Greenstone Belt, Western Australia: Insights from the Multiple Sulfur Isotopes

R. Cas, J. Hronsky, S. Beresford, 2012 .

Internal stratigraphic architecture of the komatiitic dunite-hosted MKD5 disseminated nickel sulfide deposit, Mount Keith Domain, Agnew-Wiluna Greenstone Belt, Western Australia

R. Cas, S. Beresford, M. Fiorentini, 2007 .

AN INTRUSIVE ORIGIN FOR THE KOMATIITIC DUNITE-HOSTED MOUNT KEITH DISSEMINATED NICKEL SULFIDE DEPOSIT, WESTERN AUSTRALIA

R. Cas, S. Beresford, N. Rosengren, 2005 .

Structural evolution of the Agnew–Wiluna greenstone belt, Eastern Yilgarn Craton and implications for komatiite-hosted Ni sulfide exploration

W. Bleeker, S. Beresford, P. Duuring, 2012 .