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Publications

  • 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
  • Structure and fluid migration in a late Cenozoic duplex system forming the Main Divide in the central Southern Alps, New Zealand

    Authors
    Dave Craw, C.P. Chamberlain, S.C. Cox
    Journal
    New Zealand Journal of Geology and Geophysics
    Year
    1997
    The Alpine Schist immediately west of the Main Divide of the Southern Alps is a west-dipping duplex system consisting of an imbricated stack of rock slabs, each c. 250-1000 m thick. The imbricated sta... REGISTER NOW TO SEE MORE
  • Gold mineralization as a consequence of continental collision: an example from the Southern Alps, New Zealand

    Authors
    Dave Craw, P.O. Koons
    Journal
    Earth and Planetary Science Letters
    Year
    1991
    Formation of gold-quartz veins within the Alpine Schist near the Alpine Fault was synchronous with uplift. The temperature of vein formation was greater than 320°C at a depth of ?? 4-5 km. Vein precip... REGISTER NOW TO SEE MORE
  • Southern Alps Cu-Au hydrothermal system, Westland, New Zealand

    Authors
    Dave Craw, R.D. Johnstone, M.S. Rattenbury
    Journal
    Mineralium Deposita
    Year
    1990
    The Southern Alps of New Zealand is an actively rising mountain belt which displays a thermal anomaly adjacent to the Alpine Fault, the Australian-Pacific plate boundary. Extensive fluid movement occu... REGISTER NOW TO SEE MORE