oa Minerals geophysics

References

1. Austin, J.R. and C.AFoss. 2014. The paradox of scale: Reconciling magnetic anomalies with rock magnetic properties for cost-effective mineral exploration. Journal of Applied Geophysics104:121–133.
   [Google Scholar]
2. Austin, J.R., P.W.Schmidt, C. AFoss and B.O.Patterson. 2017a. Fractional crystallization, exsolution, rapid uplift and polar reversals: Understanding the complex magnetic signatures of magmatic Ni-PGE systems. Improving exploration with petrophysics: The application of magnetic remanence and other rock physical properties to geophysical targeting.Exploration ‘17, Toronto, Canada.
   [Google Scholar]
3. Austin, J.R., S.Schmid and C.A.Foss. 2017b. Using stratiform magnetic anomalies to map near-surface architecture: insights from the Amadeus Basin. Australian Journal of Earth Sciences64(3): 353–383.
   [Google Scholar]
4. Austin, J.R., C. A.Foss and B. O.Patterson. 2017c. Challenges in ground-truthing magnetisations interpreted from magnetic field data. Improving exploration with petrophysics: The application of magnetic remanence and other rock physical properties to geophysical targeting. Exploration ‘17, Toronto, Canada.
   [Google Scholar]
5. AustinJ.R., B.O.Patterson, R.Birchall and M.Pearce. 2018. Capricorn SIEF Project: Integrated, mineralogical, petrophysical and structural characterisation - Part 4: Magnetic modelling, data integration and exploration implications. CSIRO Report EP181596.
   [Google Scholar]
6. Austin, J. and B.Crawford. 2019. Remanent magnetisation mapping: A tool for greenfields magmatic Ni-Cu-PGE exploration undercover: Part 1. Ore Geology Reviews107:457–475.
   [Google Scholar]
7. Austin, J.R. and B. O.Patterson. 2020. Deciphering deformation in ultramafic intrusions via magnetic fabric (AMS) and palaeomagnetic studies, Savannah Ni-PGE camp, NW Australia. Tectonophysics793: 228608.
   [Google Scholar]
8. Beiki, M., D. A.Clark, J. R.Austin and C. A.Foss. 2012. Estimating source location using normalised magnetic source strength calculated from magnetic gradient tensor data. Geophysics77(6): J23–J37.
   [Google Scholar]