Magnetic and gravity source models of the Gairdner Dolerites

Author:

Heath Philip1,Foss Clive2

Affiliation:

1. Geological Survey of South Australia Adelaide, SA

2. CSIRO Mineral Resources North Ryde, NSW

Publisher

Informa UK Limited

Reference6 articles.

1. Foss, C., Gouthas, G., Fabris, A., Werner, M., Katona, L., Hutchens, M., and Reed, G., 2018, Gawler Craton Airborne Geophysical Survey Region 3B, Torrens – Enhanced geophysical imagery and magnetic source depth models, Report Book 2018/00038. Department for Energy and Mining, South Australia, Adelaide.

2. Huang, Q., Kamenetsky, V., McPhie, J., Ehrig, K., Meffre, S., Maas, R., Thompson, J., Kamenetsky, M., Chambefort, I., Apukhtina, O., and Hu, Y., 2015, Neoproterozoic (ca. 820–830 Ma) mafic dykes at Olympic Dam, South Australia: Links with the Gairdner Large Igneous Province: Precambrian Research, 271, 160-172.

3. Katona, L., 2018, The Gawler Graton Airborne Survey – setting a new standard for magnetic and radiometric data in South Australia: Geological Survey of South Australia Discovery Day 2018, Presentation abstracts and posters, Report Book 2018/00034. Department of Energy and Mining, South Australia, Adelaide.

4. Naudy, H., 1971, Automatic determination of depth on aeromagnetic profiles, Geophysics, 36, pp. 717-722.

5. Shi, Z.S., 1991, An iproved Naudy-based technique for estimating depth from magnetic profiles. Exploration Geophysics, 22, pp. 357-362.

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