Interpreting geology from geophysics in poly-deformed and mineralised terranes; the Otago Schist and the Hyde-Macraes Shear Zone

Casey Catherine Blundell, Robin Armit, Laurent Ailleres, Steven Micklethwaite, Adam Martin, Peter Betts

Research output: Contribution to journalArticleResearchpeer-review

Abstract

Ore deposits are formed by a variety of processes, and mineralised host rocks possess unusual petrophysical properties in contrast to un-mineralised country rock. Mineralised systems can therefore be identified directly in geophysical data via anomalous geophysical responses. In this paper, we review the interpretation of geology from aeromagnetic and electromagnetic data relative to orogenic gold systems. As a case study, we examine the Hyde-Macraes Shear Zone in eastern Otago, New Zealand, which hosts a world-class orogenic gold system within hydrothermally altered and graphitic schist. A subtle low-resistivity anomaly in electromagnetic data correlates well with the location of the mineralised shear zone, which is otherwise indistinct in aeromagnetic data. We interpret other candidates for mineralised structures to be present in similar low-resistivity features in the south of the study area. We interpret magnetite-bearing mafic bodies, and magnetite- and pyrrhotite-rich schists to be the source of regionally extensive, isoclinally folded anomalies which are prominent features in the magnetic and electrical data and allude to the complex accretion and deformation history of the Otago Schist. Future work encompassing detailed field analyses of low-resistivity anomalies in the south of the map may reveal suitable targets for exploration.

Original languageEnglish
Number of pages23
JournalNew Zealand Journal of Geology and Geophysics
DOIs
Publication statusAccepted/In press - 1 Jan 2019

Keywords

  • aeromagnetics
  • deformation
  • frequency-domain electromagnetics (FDEM)
  • geophysical methods
  • Hyde-Macraes Shear Zone
  • Macraes
  • metamorphic belt
  • orogenic gold
  • Otago
  • structural geophysics

Cite this

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title = "Interpreting geology from geophysics in poly-deformed and mineralised terranes; the Otago Schist and the Hyde-Macraes Shear Zone",
abstract = "Ore deposits are formed by a variety of processes, and mineralised host rocks possess unusual petrophysical properties in contrast to un-mineralised country rock. Mineralised systems can therefore be identified directly in geophysical data via anomalous geophysical responses. In this paper, we review the interpretation of geology from aeromagnetic and electromagnetic data relative to orogenic gold systems. As a case study, we examine the Hyde-Macraes Shear Zone in eastern Otago, New Zealand, which hosts a world-class orogenic gold system within hydrothermally altered and graphitic schist. A subtle low-resistivity anomaly in electromagnetic data correlates well with the location of the mineralised shear zone, which is otherwise indistinct in aeromagnetic data. We interpret other candidates for mineralised structures to be present in similar low-resistivity features in the south of the study area. We interpret magnetite-bearing mafic bodies, and magnetite- and pyrrhotite-rich schists to be the source of regionally extensive, isoclinally folded anomalies which are prominent features in the magnetic and electrical data and allude to the complex accretion and deformation history of the Otago Schist. Future work encompassing detailed field analyses of low-resistivity anomalies in the south of the map may reveal suitable targets for exploration.",
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Interpreting geology from geophysics in poly-deformed and mineralised terranes; the Otago Schist and the Hyde-Macraes Shear Zone. / Blundell, Casey Catherine; Armit, Robin; Ailleres, Laurent; Micklethwaite, Steven; Martin, Adam; Betts, Peter.

In: New Zealand Journal of Geology and Geophysics, 01.01.2019.

Research output: Contribution to journalArticleResearchpeer-review

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AU - Ailleres, Laurent

AU - Micklethwaite, Steven

AU - Martin, Adam

AU - Betts, Peter

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