Potential field “worms” and models as the basis of a 3D tectonic model of the Koonenberry Belt, north-western NSW

Robert Musgrave[email protected];Geological Survey of New South Wales, NSW Department of Primary Industries PO Box 344, Hunter Region Mail Centre, NSW 2310

Yvette Poudjom Djomani[email protected];Geological Survey of New South Wales, NSW Department of Primary Industries PO Box 344, Hunter Region Mail Centre, NSW 2310

John Greenfield[email protected];Geological Survey of New South Wales, NSW Department of Primary Industries PO Box 344, Hunter Region Mail Centre, NSW 2310

Rosemary Hegarty[email protected];Geological Survey of New South Wales, NSW Department of Primary Industries PO Box 344, Hunter Region Mail Centre, NSW 2310

Stephen Dick[email protected];Geological Survey of New South Wales, NSW Department of Primary Industries PO Box 344, Hunter Region Mail Centre, NSW 2310

References

Direen, N.G., 1998, The Palaeozoic Koonenberry fold and thrust belt, western NSW; a case study in applied gravity and magnetic modelling: Exploration Geophysics, 29, 330-339.
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Lane, R., FitzGerald, D, Guillen, A., Seikel, R., and McInerney, P., 2007, Lithologically constrained inversion of magnetic and gravity data sets: Preview, 129, 11-17.
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Mills, K.J., and David, V., 2004, The Koonenberry Deep Seismic Reflection Line and geological modelling of the Koonenberry region, in western New South Wales: Report No. GS2004/185, Geological Survey of New South Wales, New South Wales Department of Mineral Resources.
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Potential field “worms” and models as the basis of a 3D tectonic model of the Koonenberry Belt, north-western NSW

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Potential field “worms” and models as the basis of a 3D tectonic model of the Koonenberry Belt, north-western NSW

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