A magnetotelluric image of the Curnamona Province and the adjacent Delamerian Orogen margin: new insights into the crustal architecture

TL;DR

This study uses new magnetotelluric data to produce a detailed 3D resistivity model of the crustal architecture in the Curnamona Province and Delamerian Orogen margin, revealing key conductive features and their geological implications.

Contribution

The paper provides the first detailed 3D resistivity model of the region, resolving previously mapped features and linking conductivity anomalies to geological processes and mineralization.

Findings

Confirmed the continuity of the ENAC conductor as the BHC into the Curnamona Province.

Identified the Wilcannia Conductor as a younger feature related to late Delamerian or Siluro-Devonian magmatism.

Suggested that conductivity anomalies are associated with large-scale trans-crustal structures influencing mineral deposits.

Abstract

We have used new magnetotelluric data collected in the Curnamona Province and the adjacent part of the Delamerian Orogen margin to image electrical conductivity structures and to inform the understanding of the crustal architecture within the regional geological context. The preferred 3D resistivity model confirms, and resolves in greater detail, crustal-scale conductive features that have been mapped by the long-period data collected at half-degree spacing as part of the Australian Lithospheric Architecture Magnetotelluric Project (AusLAMP), that is, the prominent Curnamona Province Conductor and the two Nackara Arc conductors. The new model reveals that the eastern Nackara Arc (ENAC) conductor continues as the Broken Hill Conductor (BHC) into the Curnamona Province. Regional geological considerations suggest that its formation is possibly linked to rifting/extension in the early Cambrian. Although we recognise that the east-west trending Wilcannia Conductor could be a possible continuation of the ENAC-BHC zone, integration with recently acquired deep seismic reflection data and evaluation of the geological setting lead us to suggest that they are not genetically linked. We suggest that the Wilcannia Conductor is younger and most likely is related to late Delamerian (~500 Ma) or Siluro-Devonian magmatism. Finally, these conductivity anomalies may represent large-scale trans-crustal structures that control the emplacement of low volume alkaline ultramafic magmas, and show a spatial relationship with certain mineral deposit types, suggesting a possible control on the distribution and formation of metallogenic provinces/belts in the region. This will be further investigated in future work.