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Publications

  • Sources of metals and fluids in orogenic gold deposits: Insights from the Otago and Alpine schists, New Zealand

    Authors
    Dave Craw, I.K. Pitcairn, D.A.H. Teagle, G.R. Olivo, R. Kerrich, T.S. Brewer
    Journal
    Economic Geology
    Year
    2006
    The Otago and Alpine schists of the South Island of New Zealand form a young (lt;200 Ma), lithologically monotonous, metasedimentary belt with exposures ranging from unmetamorphosed graywackes to amph... REGISTER NOW TO SEE MORE

  • Neoproterozoic structural slices in the Ross Orogen, Skelton Glacier area, South Victoria Land, Antarctica

    Authors
    Dave Craw, Y.A. Cook
    Journal
    New Zealand Journal of Geology and Geophysics
    Year
    2002
    In the Skelton Glacier area, metasedimentary basement of the Ross Orogen comprises nine structurally and lithologically distinct fault-bounded crustal slices containing varying proportions of limeston... REGISTER NOW TO SEE MORE

  • Tectonically driven fluid flow and gold mineralisation in active collisional orogenic belts: Comparison between New Zealand and western Himalaya

    Authors
    Dave Craw, P.O. Koons, T. Horton, C.P. Chamberlain
    Journal
    Tectonophysics
    Year
    2002
    Hydrothermal activity and mesothermal-styled gold mineralisation occurs near the main topographic divide of most active or young collisional mountain belts. The Southern Alps of New Zealand is used in... REGISTER NOW TO SEE MORE

  • Gold mineralization without quartz veins in a ductile-brittle shear zone, Macraes Mine, Otago Schist, New Zealand

    Authors
    Dave Craw, S.J. Windle, P.V. Angus
    Journal
    Mineralium Deposita
    Year
    1999
    Greenschist facies schist which hosts the Macraes Mine in East Otago, New Zealand has been pervasively altered by post-metamorphic (lower greenschist facies) fluids over a 120 m thick section perpendi... REGISTER NOW TO SEE MORE

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