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Conference Proceedings

PACRIM 2019

Conference Proceedings

PACRIM 2019

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Structural setting and discovery of new resources within the Hyde-Macraes Shear Zone, Macraes Mine, New Zealand

By the end of 2018, 4.9 Mozs Au had been mined from OceanaGolds Macraes mine in the South Island of New Zealand. A further 4.3 Moz remain in the gold resource implying a total gold endowment of >10 Moz.The Macraes gold deposit is located within the 1.5 km wide exposure of the Hyde-Macraes Shear Zone (HMSZ), a gently NE-dipping shear system that can be traced 20+ km along strike through the NE part of the Mesozoic Otago Schist (Figure 1). The HMSZ cuts chlorite zone quartzofeldspathic schists and is thought to have developed during late Jurassic contractional deformation along the margin of Gondwana. Mineralisation within the HMSZ occurred in the Early Cretaceous, towards the end of metamorphism, as the host schist was uplifted through the brittle-ductile transition. CITATION: Blakemore, H, Allibone, A, Craw, D, MacKenzie, D, Moore, J and Jones, P, 2019. Structural setting and discovery of new resources within the Hyde-Macraes Shear Zone, Macraes Mine, New Zealand, in Proceedings PACRIM 2019, pp 248251 (The Australasian Institute of Mining and Metallurgy: Melbourne).
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  • Structural setting and discovery of new resources within the Hyde-Macraes Shear Zone, Macraes Mine, New Zealand
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  • Published: 2019
  • PDF Size: 0.628 Mb.
  • Unique ID: P201901072

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