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https://hdl.handle.net/2440/34294
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Type: | Journal article |
Title: | Far-field continental backarc setting for the 1.80-1.67 Ga basins of northeastern Australia |
Author: | Giles, D. Betts, P. Lister, G. |
Citation: | Geology (Boulder), 2002; 30(9):823-826 |
Publisher: | Geological Soc America Inc |
Issue Date: | 2002 |
ISSN: | 0091-7613 |
Statement of Responsibility: | David Giles, Peter Betts, and Gordon Lister |
Abstract: | The 1.80–1.67 Ga volcano-sedimentary basins of northeastern Australia, preserved in the Mount Isa inlier, McArthur basin, and Georgetown inlier, have been a cornerstone of nonuniformitarian “intracontinental” tectonic models of the Australian Proterozoic. However, geochronological data show that major tectonothermal events within the basins coincided with significant tectonic events that occurred along a complex convergent plate boundary that developed on the southern margin of the proto–Australian continent. These data imply a paired evolution, whereby thermal events were shared and plate-margin stresses were propagated (to 1500 km) into the plate interior. We propose a tectonic model in which the 1.80–1.67 Ga northeastern Australian basins occupied a wide region of intermittently extending continental crust in the overriding plate of a long-lived subduction system—effectively a far-field continental backarc setting. The combined effects of slab rollback, accretion, and enhanced subcontinental convection produced an environment of episodic extension, transient shortening, elevated heat flow, and magmatism. |
Keywords: | Proterozoic, Australia, continental backarc, plate tectonics |
Description: | Copyright © 2002 Geological Society of America |
DOI: | 10.1130/0091-7613(2002)030<0823:FFCBSF>2.0.CO;2 |
Published version: | http://dx.doi.org/10.1130/0091-7613(2002)030%3C0823:ffcbsf%3E2.0.co;2 |
Appears in Collections: | Aurora harvest 6 Earth and Environmental Sciences publications |
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