Conference Proceedings
PACRIM 2019
Conference Proceedings
PACRIM 2019
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).
Contributor(s):
H Blakemore, A Allibone, D Craw, D MacKenzie, J Moore, P Jones
-
Structural setting and discovery of new resources within the Hyde-Macraes Shear Zone, Macraes Mine, New ZealandPDFThis product is exclusive to Digital library subscription
-
Structural setting and discovery of new resources within the Hyde-Macraes Shear Zone, Macraes Mine, New ZealandPDFNormal price $16.50Member price from $0.00
Fees above are GST inclusive
PD Hours
Approved activity
- Published: 2019
- PDF Size: 0.628 Mb.
- Unique ID: P201901072