Paleomagnetic testing of the Lachlan Orocline hypothesis: Overprinting of remanence in Paleozoic rocks of the Lachlan Orogen in southeast Australia
Author:
Affiliation:
1. Centre for Ore Deposit and Earth Sciences, University of Tasmania, Hobart, Australia
2. Geological Survey of New South Wales, Department of Regional NSW, Newcastle, Australia
Funder
Australian Research Council, Rio Tinto
Heron Resources
Alkane Resources
Evolution Mining
IMEX Consulting
Emmerson Resources
Anglo Gold Ashanti
Sandfire Resources
New South Resources
Northparkes Mines
Geological Survey of Victoria
Geological Survey of New South Wales
Mineral Resources Tasmania
University of Tasmania
Macquarie University
Curtin University
Publisher
Informa UK Limited
Subject
General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)
Link
https://www.tandfonline.com/doi/pdf/10.1080/08120099.2021.1918246
Reference98 articles.
1. Geomagnetic polarity bias patterns through the Phanerozoic
2. Rock magnetism of Late Neogene and Pleistocene deep-sea sediments: Relationship to sediment source, diagenetic processes, and sediment lithology
3. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic
4. Exotic crustal block accretion to the eastern Gondwanaland margin in the Late Cambrian–Tasmania, the Selwyn Block, and implications for the Cambrian–Silurian evolution of the Ross, Delamerian, and Lachlan orogens
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2. 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
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