Paleomagnetism of the Acraman–Bunyeroo meteorite impact ejecta zone in the South Flinders Ranges region, South Australia

References

• Bird, M. I., & Chivas, A. R. (1989). Stable-isotope geochronology of the Australian regolith. Geochimica et Cosmochimica Acta, 53(12), 3239–3256. https://doi.org/10.1016/0016-7037(89)90104-X
   Web of Science ®Google Scholar
• Butler, R. F. (1992). Paleomagnetism: Magnetic domains to geologic terranes. Blackwell Scientific Publications. https://doi.org/10.1007/978-3-540-27980-8_4
   Google Scholar
• Collinson, D. W. (1983). Methods in rock magnetism and palaeomagnetism. Chapman and Hall. https://doi.org/10.1007/978-94-015-3979-1
   Google Scholar
• Farrand, M. G. (1995). Mesozoic igneous rocks. In J. F. Drexel & W. V. Preiss (Eds.), The geology of South Australia, Volume 2, The Phanerozoic (pp. 148–149). Geological Survey of South Australia Bulletin 54/2.
   Google Scholar
• Fisher, R. A. (1953). Dispersion on a sphere. Proceedings of the Royal Society of London, Series A, 217(1130), 295–305. https://doi.org/10.1098/rspa.1953.0064
   Google Scholar
• Gostin, V. A., Haines, P. W., Jenkins, R. J. F., Compston, W., & Williams, I. S. (1986). Impact ejecta horizon within late Precambrian shales, Adelaide Geosyncline, South Australia. Science, 233(4760), 198–200. https://doi.org/10.1126/science.233.4760.198
   PubMed Web of Science ®Google Scholar
• Jagodzinski, E. A., Reid, A. J., Crowley, J. L., Wade, C. E., & Curtis, S. (2023). Precise zircon U–Pb dating of the Mesoproterozoic Gawler large igneous province, South Australia. Results in Geochemistry, 10, 100020. https://doi.org/10.1016/j.ringeo.2022.100020
   Google Scholar
• Kent, J. T., Briden, J. C., & Mardia, K. V. (1983). Linear and planar structure in ordered multivariate data as applied to progressive demagnetization of palaeomagnetic remanence. Geophysical Journal International, 75(3), 593–621. https://doi.org/10.1111/j.1365-246X.1983.tb05001.x
   Google Scholar
• Lloyd, J. C., Blades, M. L., Counts, J. W., Collins, A. S., Amos, K. J., Wade, B. P., Hall, J. W., Hore, S., Ball, A. L., Shahin, S., & Drabsch, M. (2020). Neoproterozoic geochronology and provenance of the Adelaide Superbasin. Precambrian Research, 350, 105849. https://doi.org/10.1016/j.precamres.2020.105849
   Web of Science ®Google Scholar
• Lowrie, W. (1990). Identification of ferromagnetic minerals in a rock by coercivity and unblocking temperature properties. Geophysical Research Letters, 17(2), 159–162. https://doi.org/10.1029/GL017i002p00159
   Web of Science ®Google Scholar
• McDougall, I., & Wellman, P. (1976). Potassium argon ages for some Australian Mesozoic igneous rocks. Journal of the Geological Society of Australia, 23(1), 1–9. https://doi.org/10.1080/00167617608728916
   Google Scholar
• Milnes, A. R., Cooper, B. J., & Cooper, J. A. (1982). The Jurassic Wisanger basalt of Kangaroo Island, South Australia. Transactions of the Royal Society of South Australia, 106, 1–13.
   Google Scholar
• Minguez, D., & Kodama, K. P. (2017). Rock magnetic chronostratigraphy of the Shuram carbon isotope excursion: Wonoka Formation, Australia. Geology, 45(6), 567–570. https://doi.org/10.1130/G38572.1
   Web of Science ®Google Scholar
• Schmidt, P. W. (1976). A new palaeomagnetic investigation of Mesozoic igneous rocks in Australia. Tectonophysics, 33(1-2), 1–13. https://doi.org/10.1016/0040-1951(76)90048-2
   Web of Science ®Google Scholar
• Schmidt, P. W., & Clark, D. A. (2000). Paleomagnetism, apparent polar-wander path, & paleolatitude. In J. J. Veevers (Ed.), Billion-year earth history of Australia and neighbours in Gondwanaland (pp. 12–17). GEMOC Press.
   Google Scholar
• Schmidt, P. W., & Williams, G. E. (1991). Palaeomagnetic correlation of the Acraman impact structure and the Late Proterozoic Bunyeroo ejecta horizon, South Australia. Australian Journal of Earth Sciences, 38(3), 283–289. https://doi.org/10.1080/08120099108727972
   Web of Science ®Google Scholar
• Schmidt, P. W., & Williams, G. E. (1996). Palaeomagnetism of the ejecta-bearing Bunyeroo Formation, late Neoproterozoic, Adelaide fold belt, and the age of the Acraman impact. Earth and Planetary Science Letters, 144(3-4), 347–357. https://doi.org/10.1016/S0012-821X(96)00169-0
   Web of Science ®Google Scholar
• Till, J. L., & Nowaczyk, N. (2018). Authigenic magnetite formation from goethite and hematite and chemical remanent magnetization acquisition. Geophysical Journal International, 213(3), 1818–1831. https://doi.org/10.1093/gji/ggy083
   Web of Science ®Google Scholar
• Wallace, M. W., Gostin, V. A., & Keays, R. R. (1990). Acraman impact ejecta and host shales: Evidence for low temperature mobilization of iridium and other platinoids. Geology, 18(2), 132–135. https://doi.org/10.1130/0091-7613(1990)018%3C0132:AIEAHS%3E2.3.CO;2
   Web of Science ®Google Scholar
• Williams, G. E. (1986). The Acraman impact structure: Source of ejecta in late Precambrian shales, South Australia. Science, 233(4760), 200–203. https://doi.org/10.1126/science.233.4760.200
   PubMed Web of Science ®Google Scholar
• Williams, G. E., & Gostin, V. A. (2005). Acraman–Bunyeroo impact event (Ediacaran), South Australia, and environmental consequences: Twenty-five years on. Australian Journal of Earth Sciences, 52(4-5), 607–620. https://doi.org/10.1080/08120090500181036
   Web of Science ®Google Scholar