ArticleSm-Nd isotopic evidence for the provenance of sediments from the Adelaide Fold Belt and southeastern Australia with implications for episodic crustal addition
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2020, Gondwana ResearchCitation Excerpt :The Kanmantoo Group had more negative εNd values and slightly older model ages. Neither interval was a good match for the even more negative εNd values and older model ages derived from Gawler Craton rocks, although Turner et al. (1993a) and Turner et al. (1993b) suggested that the Kanmantoo isotopic signature could be explained by the mixing of Gawler Craton derived sediment with reworked Neoproterozoic material. The SmNd and Sr isotopic signature of the Kanmantoo Group was further investigated by Haines et al. (2009) who analysed closely associated mudstone–sandstone and pelite–psammite pairs (collected <50 cm apart stratigraphically) throughout the group.
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Present address: Department of Earth Sciences, Open University, Milton Keynes, MK7 6AA, England.