Changes in Relative Plate Motion during the Isan Orogeny (1670-1500 Ma) and Implications for Pre-Rodinia Reconstructions
Author:
Affiliation:
1. School of Earth and Environmental Science; James Cook University; Townsville QLD 4811 Australia
2. Geology Department; Beni-Suef University; Beni-Suef 62511 Egypt
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/1755-6724.12644/fullpdf
Reference112 articles.
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2. Radical changes in bulk shortening directions during orogenesis: significance for progressive development of regional folds and thrusts;Abu Sharib;Precambrian Research,2011
3. Polymetamorphism accompanied switching in horizontal shortening during Isan Orogeny: Example from the Eastern Fold Belt, Mount Isa Inlier, Australia;Abu Sharib;Tectonophysics,2013
4. Correlating deformation in Variscan NW Iberia usingporphyroblasts; implications for the Ibero-Armorican Arc;Aerden;Journal of Structural Geology,2004
5. Multi-stage mountain building vs. relative plate motions in the Betic Cordillera deduced from integrated microstructural and petrological analysis of porphyroblast inclusion trails;Aerden;Tectonophysics,2013
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1. Evidence for a 1750–1710 Ma orogenic event, the Wonga Orogeny, in the Mount Isa Inlier, Australia: Implications for the tectonic evolution of the North Australian Craton and Nuna Supercontinent;Precambrian Research;2022-02
2. 1750–1710 Ma deformation along the eastern margin of the North Australia Craton;Precambrian Research;2021-02
3. Low Angle Normal-Sense Shear Zones, Folds and Wrench Faults During the Post-Amalgamation Stage of the Arabian-Nubian Shield;The Geology of the Arabian-Nubian Shield;2021
4. Extension-related buttress-like folds, the western side of the Gulf of Suez rift, Egypt;International Journal of Earth Sciences;2017-02-28
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