405m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

580m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

800m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

885m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

1280m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

This model was produced by The South Australian Centre for Mineral Exploration Under Cover (CMXUC), a collaborative research initiative of the Government of South Australia and the University of Adelaide. The northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Adelaide Geosyncline during the Neoproterozoic to Early Cambrian. Despite numerous studies, the geometry and evolution of the basin is still not well understood. This project aims to reconstruct the evolution from the Neoproterozoic to Quaternary and to model the geometry of the basement under cover.

4730m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

6580m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

8380m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.

12530m depth slice from the 3-D resistivity model derived from magnetotelluric (MT) data collected from 231 sites in the Curnamona and Delamerian Region. The resistivity model can be used to enhance the understanding of the geodynamics and mineral potential in the Curnamona Province and Delamerian Orogen.