Publications

Currently searching 17 publications

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Publications

  • Modelling the role of graphite in development of a mineralised mid-crustal shear zone, Macraes mine, New Zealand

    Authors
    Dave Craw, P. Upton
    Journal
    Earth and Planetary Science Letters
    Year
    2008
    The Hyde-Macraes Shear Zone (HMSZ) is a mineralised low-angle shear within the Otago Schist traceable for ?? 30 km with a NW strike. It is being actively mined along 12 km of this strike, producing > ... REGISTER NOW TO SEE MORE

  • 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

  • Integrated outcrop, drill core, borehole and seismic stratigraphic architecture of a cyclothemic, shallow-marine depositional system, Wanganui Basin, New Zealand

    Authors
    Brad Field, G.S. Wilson, T.R. Naish, H. Zhu, A. Melhuish, R.M. Carter, S.T. Abbott, S. Edwards, B.V. Alloway, F. Niessen, A. Barker, G.H. Browne, G. Maslen
    Journal
    Journal of the Royal Society of New Zealand
    Year
    2005
    Late Pliocene to mid-Pleistocene (c. 2.1-0.4 Ma) strata exposed in the, now classical, Nukumaru and Castlecliff coastal cliff sections north-west of Wanganui comprise 25, 6th (41 ka) order and 5th (10... REGISTER NOW TO SEE MORE

  • Petrogenesis of diachronous mixed siliciclastic-carbonate megafacies in the cool-water Oligocene Tikorangi Formation, Taranaki Basin, New Zealand

    Authors
    Peter Kamp, C.S. Nelson, S.D. Hood
    Journal
    New Zealand Journal of Geology and Geophysics
    Year
    2003
    The Oligocene (Whaingaroan-Waitakian) Tikorangi Formation is a totally subsurface, lithostratigraphically complex, mixed siliciclastic-limestone-rich sequence forming an important fracture reservoir w... REGISTER NOW TO SEE MORE

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