Disputed tectonic setting for the late Silurian–early Carboniferous development of the northern New England Orogen: detrital zircon ages suggest a continental margin arc association
Author:
Affiliation:
1. Department of Earth and Environmental Sciences, James Cook University, Townsville, QLD, Australia
2. School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, Australia
Publisher
Informa UK Limited
Link
https://www.tandfonline.com/doi/pdf/10.1080/08120099.2024.2360947
Reference102 articles.
1. Devonian Crustal Stretching in the Northern Tasmanides (Australia) and Implications for Oroclinal Bending
2. Archean and Paleoproterozoic zircons in Paleozoic sandstones in southern New Zealand: evidence for remnant Nuna supercontinent and Ur continent rocks within Zealandia
3. Adams, C. J., Wormald, R., & Henderson, R. A. (2013). Detrital zircons from the Hodgkinson Formation: Constraints on its maximum depositional age and provenance. In P. A. Jell (Ed.), Geology of Queensland (pp. 239–241). Geological Survey of Queensland.
4. Gamilaroi Terrane: A Devonian rifted intra-oceanic island-arc assemblage, NSW, Australia.
5. Geochronology and geochemistry of the Devonian Gumbardo Formation (Adavale Basin): evidence for cratonisation of the Central Thomson Orogen by the Early Devonian
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