Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/13790
Citations
Scopus Web of Science® Altmetric
?
?
Type: Journal article
Title: U-Pb ages from the Harts Range, central Australia: evidence for Early Ordovician extension and constraints on Carboniferous metamorphism
Author: Hand, M.
Mawby, J.
Kinny, P.
Foden, J.
Citation: Journal of the Geological Society, 1999; 156(4):715-730
Publisher: The Geological Society
Issue Date: 1999
ISSN: 0016-7649
2041-479X
Abstract: Sensitive high-resolution ion microprobe (SHRIMP) U–Pb analyses of monazite and zircon from the Harts Range indicate the southeastern Arunta Inlier has been affected by two major Palaeozoic tectonothermal events. During the early Ordovician (467 ± 8 Ma), regional deformation produced a sub-horizontal upper amphibolite-facies (> 700°C and 7 kbar) shear fabric that overprinted c. 800°C migmatitic assemblages. In the intracratonic Amadeus Basin south of the Harts Range region, subsidence rates increased in the early Ordovician with the accumulation of easterly, and southerly, derived mature sediments. This is contrary to what would be expected if deformation in the Harts Range region occurred in a compressional setting, and suggests that the early Ordovician deformation may have occurred in an extensional intraplate setting. The terrain remained at depth until the mid-Carboniferous when up to 20 km of exhumation occurred during the latter stages of the intracratonic Devonian to Carboniferous (400–300 Ma) Alice Springs Orogeny. Monazite U–Pb data indicates the structurally lowest parts of the terrain were at c. 6 bar and ≥c. 600°C at 343 ± 8 Ma, and subsequently underwent high-temperature decompression, resulting in overprinting of the kyanite-grade assemblages with sillimanite-bearing assemblages during south-directed thrusting. During exhumation, pegmatite emplaced in the southeastern Harts Range at 330 ± 6 Ma (zircon U–Pb) was strongly deformed at temperatures around 560°C and depths around 15 km. The U–Pb data from the Harts Range indicate that the record of intraplate deformation in central Australia was more complex than previously thought.
Keywords: Ordovician; Alice Springs Orogeny; U–Pb; monazite; intraplate deformation
Rights: © 1999 Geological Society of London
RMID: 0030003572
DOI: 10.1144/gsjgs.156.4.0715
Published version: http://jgs.geoscienceworld.org/cgi/content/abstract/156/4/715
Appears in Collections:Geology & Geophysics publications
Environment Institute publications

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.