Research paperGeological history of the early Proterozoic Paraburdoo Hinge Zone, Western Australia
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Reply to comment on “Bekker, A., Krapež, B., Karhu, J.A., 2020. Correlation of the stratigraphic cover of the Pilbara and Kaapvaal cratons recording the lead up to Paleoproterozoic Icehouse and the GOE. Earth-Science Reviews, 211, 103,389” by Pascal Philippot, Bryan A. Killingsworth, Jean-Louis Paquette, Svetlana Tessalina, Pierre Cartigny, Stefan V. Lalonde, Christophe Thomazo, Janaina N. Ávila, Vincent Busigny
2021, Earth-Science ReviewsCitation Excerpt :We note that the correlation scheme Philippot et al. (2018, 2021) advocated for the Pilbara Craton/Hamersley Province is partially based on outdated and erroneous information. Firstly, while they claim that they show the lithostratigraphy for the Turee Creek Basin, they show the lithostratigraphy of the McGrath Trough (sensu Horwitz, 1982; Martin et al., 2000), which combines successions pertaining to the Turee Creek Basin and the overlying, but tectonogenetically unrelated, Horseshoe Basin as defined by Krapez (1996, 1997) and by Krapež et al. (2015, 2017). The correct nomenclature and lithostratigraphic components, if using the tectonostratigraphic term Turee Creek Basin, are shown here in Fig. 1 and by Bekker et al. (2020, their fig. 2).
U-Pb detrital zircon geochronology of the Turee Creek Group, Hamersley Basin, Western Australia: Timing and correlation of the Paleoproterozoic glaciations
2018, Precambrian ResearchCitation Excerpt :More investigations are required to determine the provenance of these quartzites. Depositional settings of the TCG have been inferred to be either a retro-arc foreland basin (e.g., Horwitz, 1982; Blake and Barley, 1992; Powell et al., 1999; Martin et al., 2000; Krapež et al., 2017) or an intracontinental basin (Van Kranendonk et al., 2015) both developed in a compressive tectonic context. Whereas the Beasley River Quartzite (part of the lower Wyloo Group) have mostly been suggested to have been deposited in an intracontinental failed rift basin (Taylor et al., 2001; Müller et al., 2005; Krapež et al., 2015).
A tale of two basins? Stratigraphy and detrital zircon provenance of the Palaeoproterozoic Turee Creek and Horseshoe basins of Western Australia
2017, Precambrian ResearchCitation Excerpt :Ocean opening was to the northwest and southwest, so that the Pilbara Craton was bordered to the northwest and southwest by ocean basins (Blake and Barley, 1992). The southwestern margin of the Hamersley Province was converted to an active margin from ∼2500 Ma involving back-arc bimodal magmatism at ∼2450 Ma (Woongarra Volcanics on Fig. 2) that was followed conformably by retroarc-basin subsidence (Horwitz, 1982; Blake and Barley, 1992; Krapez, 1996; Barley et al., 1997; Powell et al., 1999; Martin et al., 2000), presumably behind a back-arc magmatic fold-thrust belt. The tectonic history of the Hamersley Province after ∼2450 Ma is controversial, but there is broad agreement that retroarc-basin subsidence was followed by ocean closure (Ophthalmia Orogeny) and then renewed subsidence (Ashburton Province) prior to the Ashburton Orogeny (Powell and Horwitz, 1994; Krapez, 1996, 1997, 1999; Taylor et al., 2001; Evans et al., 2003; Müller et al., 2005).