Paleomagnetism of the Carboniferous Gresford Block, Tamworth Belt, southern New England Orogen: minor counter-clockwise rotation of a primary arc segment
Author:
Affiliation:
1. Research School of Earth Sciences, The Australian National University, Acton, ACT 2601, Australia
Publisher
Informa UK Limited
Subject
General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)
Link
https://www.tandfonline.com/doi/pdf/10.1080/08120099.2020.1674381
Reference197 articles.
1. Orogen-perpendicular structures in the central Tasmanides and implications for the Paleozoic tectonic evolution of eastern Australia
2. Devonian Crustal Stretching in the Northern Tasmanides (Australia) and Implications for Oroclinal Bending
3. Haematite pigmentation events and palaeomagnetic recording: implications from the Pilbara Print Stone, Western Australia
4. Agro, A. (2014). Localization of the source of large silicic ignimbrites through magnetic techniques: Applications in Turkey (Unpublished PhD thesis). Earth Sciences, Université Blaise Pascal, Clermont-Ferrand II, France.
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1. Matching mid-to-latest Carboniferous pole path segments for eastern Australia and northern Armorica indicate a late Carboniferous Pangea-B configuration and a mid Carboniferous inertial interchange true polar wander event;Earth-Science Reviews;2023-09
2. Paleomagnetism of the Carboniferous–Permian Myall blocks, Tamworth Belt, southern New England Orogen: Permian counterclockwise rotations and Triassic clockwise rotation;Australian Journal of Earth Sciences;2021-11-03
3. Paleomagnetic testing of the Lachlan Orocline hypothesis: Overprinting of remanence in Paleozoic rocks of the Lachlan Orogen in southeast Australia;Australian Journal of Earth Sciences;2021-06-08
4. A geomagnetic polarity timescale for the Carboniferous;Geological Society, London, Special Publications;2020-12-07
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