Publication Cover
Australian Journal of Earth Sciences
An International Geoscience Journal of the Geological Society of Australia
Volume 64, 2017 - Issue 2
477
Views
21
CrossRef citations to date
0
Altmetric
Original Articles

Paleomagnetism and U–Pb geochronology of the Black Range dykes, Pilbara Craton, Western Australia: a Neoarchean crossing of the polar circle

, &
Pages 225-237 | Received 10 Dec 2016, Accepted 29 Jan 2017, Published online: 01 Mar 2017

References

  • Arndt, N. T., Bruzak, G., & Reischmann, T. (2001). The oldest continental and oceanic plateaus: Geochemistry of basalts and komatiites of the Pilbara Craton, Australia. In R. E. Ernst & K. L. Buchan (Eds.), Mantle plumes: Their identification through time (pp. 359–387). 359–387. Boulder, Co: Geological Society of America Special Paper, 352.
  • Arndt, N. T., Nelson, D. R., Compston, W., Trendall, A. F., & Thorne, A. M. (1991). The age of the Fortescue Group, Hamersley Basin, Western Australia, from ion microprobe zircon U–Pb results. Australian Journal of Earth Sciences, 38, 261–281.
  • Blake, T. S. (1984). Evidence for stabilization of the Pilbara Block, Australia. Nature, 307, 721–723.
  • Blake, T. S. (1993). Late Archaean crustal extension, sedimentary basin formation, flood basalt volcanism and continental rifting: The Nullagine and Mount Jope Supersequences, Western Australia. Precambrian Research, 60, 185–241.
  • Blake, T. S., Buick, R., Brown, S. J. A., & Barley, M. E. (2004). Geochronology of a Late Archaean flood basalt province in the Pilbara Craton, Australia: Constraints on basin evolution, volcanic and sedimentary accumulation, and continental drift rates. Precambrian Research, 133, 143–173.
  • Bleeker, W. (2003). The late Archean record: A puzzle in ca. 35 pieces. Lithos, 71, 99–134.
  • Bradley, K., Weiss, B. P., & Buick, R. (2015). Records of geomagnetism, climate, and tectonics across a Paleoarchean erosion surface. Earth and Planetary Science Letters, 419, 1–13.
  • Cheney, E. S. (1996). Sequence stratigraphy and plate tectonic significance of the Transvaal succession of southern Africa and its equivalent in Western Australia. Precambrian Research, 79, 3–24.
  • de Kock, M. O., Evans, D. A. D., & Beukes, N. J. (2009). Validating the existence of Vaalbara in the Neoarchean. Precambrian Research, 174, 145–154.
  • Embleton, B. J. J. (1972). The palaeomagnetism of some Proterozoic–Cambrian sediments from the Amadeus Basin, central Australia. Earth and Planetary Science Letters, 17, 217–226.
  • Embleton, B. J. J. (1978). The palaeomagnetism of 2400 m.y. old rocks from the Australian Pilbara craton and its relation to Archaean–Proterozoic tectonics. Precambrian Research, 6, 275–291.
  • Evans, D. A. D. (2013). Reconstructing pre-Pangean supercontinents. Geological Society of America Bulletin, 125, 1735–1751.
  • Fisher, R. A. (1953). Dispersion on a sphere. Proceedings Royal Society A, 217, 295–305.
  • Fisher, N. I., Lewis, T., & Embleton, B. J. J. (1987). Statistical analysis of spherical data. Cambridge, UK: Cambridge University Press, 313 pp.
  • Gerstenberger, H., & Haase, G. (1997). A highly effective emitter substance for mass spectrometric Pb isotope ratio determinations. Chemical Geology, 136, 309–312.
  • Gumsley, A., Olsson, J., Söderlund, U., de Kock, M., Hofmann, A., & Klausen, M. (2015). Precise U–Pb baddeleyite age dating of the Usushwana Complex, southern Africa—Implications for the Mesoarchaean magmatic and sedimentological evolution of the Pongola Supergroup, Kaapvaal Craton. Precambrian Research, 267, 174–185.
  • Hall, C. E. (2005). SHRIMP U–Pb depositional age for the lower Hardey Formation: Evidence for diachronous deposition of the lower Fortescue Group in the southern Pilbara region, Western Australia. Australian Journal of Earth Sciences, 52, 403–410.
  • Heaman, L. M., & LeCheminant, A. N. (1993). Paragenesis and U–Pb systematics of baddeleyite (ZrO2). Chemical Geology, 110, 95–126.
  • Hickman, A. H. (1983). Geology of the Pilbara Block and its environs. Western Australia Geological Survey, Bulletin 127, Perth, WA: Western Australia Geological Survey, 268 p.
  • Hickman, A. H. ( compiler) (2007). Nullagine. Western Australia Geological Survey 1:250 000 Geological Map Sheet SF 51-05 (3rd ed.). Perth, WA: Western Australia Geological Survey.
  • Hickman, A. H. ( compiler) (2010). Marble Bar. Western Australia Geological Survey 1:250 000 Geological Map Sheet SF 50-8 (3rd ed.). Perth, WA: Western Australia Geological Survey.
  • Hickman, A. H. (2012). Review of the Pilbara Craton and Fortescue Basin, Western Australia: Crustal evolution providing environments for early life. Island Arc, 21, 1–31.
  • Hickman, A. H. ( compiler) (2013). North Shaw. Western Australia Geological Survey 1:100 000 Geological Map Sheet 2755 (2nd ed.). Perth, WA: Western Australia Geological Survey.
  • Hickman, A. H., & Lipple, S. L. (1978). Marble Bar. Western Australia Geological Survey 1:250 000 Geological Series Explanatory Notes. Perth, WA: Western Australia Geological Survey, 24 pp.
  • Hickman, A. H., & Van Kranendonk, M. V. ( compilers) (2008). Marble Bar. Western Australia Geological Survey 1:100 000 Geological Map Sheet 2855 (1st ed.). Perth, WA: Western Australia Geological Survey.
  • Irving, E., & Green, R. (1958). Polar movement relative to Australia. Geophysical Journal of the Royal Astronomical Society, 1, 64–72.
  • Kirschvink, J. L. (1980). The least squares line and plane and the analysis of paleomagnetic data. Geophysical Journal of the Royal Astronomical Society, 62, 699–718.
  • Lewis, J. D., Rosman, K. J. R., & de Laeter, J. R. (1975). The age and metamorphic effects of the Black Range dolerite dyke. Western Australia Geological Survey, Annual Report for the Year 1974 (pp. 80–88). Perth, WA: Western Australia Geological Survey.
  • Li, Z.-X., & Evans, D. A. D. (2011). Late Neoproterozoic 40° intraplate rotation within Australia allows for a tighter-fitting and longer-lasting Rodinia. Geology, 39, 39–42.
  • Li, Z. X., Powell, C. McA., & Thrupp, G. A. (1990). Australian Palaeozoic palaeomagnetism and tectonics–II. A revised apparent polar wander path and palaeogeography. Journal of Structural Geology, 12, 567–575.
  • Lipple, S. L. (1975). Definitions of new and revised stratigraphic units of the Eastern Pilbara Region. Western Australia Geological Survey, Annual Report for the Year 1974 (pp. 58–63). Perth, WA: Western Australia Geological Survey.
  • Ludwig, K. R. (2001). Isoplot: A Geochronological Toolkit for Microsoft Excel, Berkeley Geochronology Center, USA, Special Publication No. 1a. Berkeley, Cal: University of California.
  • Pidgeon, R. T. (1984). Geochronological constraints on early volcanic evolution of the Pilbara Block, Western Australia. Australian Journal of Earth Sciences, 31, 237–242.
  • Rainbird, R. H., & Ernst, R. E. (2001). The sedimentary record of mantle-plume uplift. In R. E. Ernst & K. L. Buchan (Eds.), Mantle plumes: Their identification through time (pp. 227–245). Boulder, Co: Geological Society of America Special Paper, 352.
  • Rasmussen, B., Fletcher, I. R., & Sheppard, S. (2005). Isotopic dating of the migration of a low-grade metamorphic front during orogenesis. Geology, 33, 773–776.
  • Schmidt, P. W. (1993). Paleomagnetic cleaning strategies. Physics of the Earth and Planetary Interiors, 76, 169–178.
  • Schmidt, P. W., & Embleton, B. J. J. (1985). Prefolding and overprint magnetic signatures in Precambrian (∼2.9–2.7 Ga) igneous rocks from the Pilbara Craton and Hamersley Basin, NW Australia. Journal of Geophysical Research, 90, 2967–2984.
  • Shipunov, S. V., Muraviev, A. A., & Bazhenov, M. L. (1998). A new conglomerate test in palaeomagnetism. Geophysical Journal International, 133, 721–725.
  • Smith, R. E., Perdrix, J. L., & Parks, T. C. (1982). Burial metamorphism in the Hamersley Basin, Western Australia. Journal of Petrology, 23, 75–102.
  • Söderlund, U., & Johansson, L. (2002). A simple way to extract baddeleyite (ZrO2). Geochemistry Geophysics Geosystems, 3, 1–7.
  • Stacey, J. S., & Kramers, J. D. (1975). Approximation of terrestrial lead isotope evolution by a two stage model. Earth and Planetary Science Letters, 26, 207–221.
  • Strik, G. H. M. A. (2004). Palaeomagnetism of late Archaean flood basalt terrains: Implications for early Earth geodynamics and geomagnetism (PhD thesis). Geologica Ultraiectina, Mededelingen van de Faculteit Geowetenschappen Universiteit Utrecht, Utrecht, Netherlands , 242, 160 pp.
  • Strik, G., Blake, T. S., Zegers, T. E., White, S. H., & Langereis, C. G. (2003). Palaeomagnetism of flood basalts in the Pilbara Craton, Western Australia: Late Archaean continental drift and the oldest known reversal of the geomagnetic field. Journal of Geophysical Research, 108, doi:10.1029/2003JB002475
  • Sumita, I., Hatakeyama, T., Yoshihara, A., & Hamano, Y. (2001). Paleomagnetism of late Archean rocks of Hamersley basin, Western Australia and the paleointensity at early Proterozoic. Physics of the Earth and Planetary Interiors, 128, 223–241.
  • Thorne, A. M., & Trendall, A. F. (2001). Geology of the Fortescue Group, Pilbara Craton, Western Australia. Perth, WA: Western Australia Geological Survey, Bulletin, 144, 249 pp.
  • Trendall, A. F. (1983). The Hamersley Basin. In A. F. Trendall & R. C. Morris (Eds.), Iron-formation: Facts and problems (pp. 69–129). Amsterdam: Elsevier.
  • Van der Voo, R. (1990). The reliability of paleomagnetic data. Tectonophysics, 184, 1–9.
  • Van Kranendonk, M. J. (2000). Geology of the North Shaw 1:100 000 Sheet. Western Australia Geological Survey 1:100 000 Geological Series Explanatory Notes. Perth, WA: Western Australia Geological Survey, 86 pp.
  • Van Kranendonk, M. J., Bleeker, W., & Ketchum, J. (2006b). Phreatomagmatic boulder conglomerates at the tip of the ca 2772 Ma Black Range dolerite dyke, Pilbara Craton, Western Australia. Australian Journal of Earth Sciences, 53, 617–630.
  • Van Kranendonk, M. J., Hickman, A. H., Smithies, R. H., Williams, I. R., Bagas, L., & Farrell, T. R. (2006a). Revised lithostratigraphy of Archean supracrustal and intrusive rocks in the northern Pilbara Craton, Western Australia. Western Australia Geological Survey, Record, 2006/15. Perth, WA: Western Australia Geological Survey, 57 pp.
  • Van Kranendonk, M. J., & Kirkland, C. L. (2016). Conditioned duality of the Earth system: Geochemical tracing of the supercontinent cycle through Earth history. Earth-Science Reviews, 160, 171–187.
  • Verwey, E. J. W. (1939). Electronic conduction of magnetite (Fe3O4) and its transition point at low-temperature. Nature, 44, 327–328.
  • Williams, H., Hoffman, P. F., Lewry, J. F., Monger, J. W. H., & Rivers, T. (1991). Anatomy of North America: Thematic geologic portrayals of the continent. Tectonophysics, 187, 117–134.
  • Wingate, M. T. D. (1999). Ion microprobe baddeleyite and zircon ages for Late Archaean mafic dykes of the Pilbara Craton, Western Australia. Australian Journal of Earth Sciences, 46, 493–500.
  • Wingate, M. T. D., Pisarevsky, S. A., & Evans, D. A. D. (2002). Rodinia connections between Australia and Laurentia: No SWEAT, no AUSWUS? Terra Nova, 14, 121–128.
  • Zegers, T. E., de Wit, M. J., Dann, J., & White, S. H. (1998). Vaalbara, Earth's oldest assembled continent? A combined structural, geochronological, and palaeomagnetic test. Terra Nova, 10, 250–259.

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.