Please use this identifier to cite or link to this item: http://hdl.handle.net/2381/38291
Title: Spatial and temporal patterns of Australian dynamic topography fromRiver Profile Modeling
Authors: Czarnota, K.
Roberts, G. G.
White, N. J.
Fishwick, Stewart
First Published: 18-Feb-2014
Publisher: American Geophysical Union (AGU), Wiley
Citation: Journal of Geophysical Research. Solid Earth, 2014, 119 (2), pp. 1384-1424 (41)
Abstract: Despite its importance, the temporal and spatial evolution of continental dynamic topography is poorly known. Australia's isolation from active plate boundaries and its rapid northward motion within a hot spot reference frame make it a useful place to investigate the interplay between mantle convection, topography, and drainage. Offshore, dynamic topography is relatively well constrained and can be accounted for by Australia's translation over the mantle's convective circulation. To build a database of onshore constraints, we have analyzed an inventory of longitudinal river profiles, which is sensitive to uplift rate history. Using independently constrained erosional parameters, we determine uplift rates by minimizing the misfit between observed and calculated river profiles. Resultant fits are excellent and calculated uplift histories match independent geologic constraints. We infer that western and central Australia underwent regional uplift during the last 50 Myr and that the Eastern Highlands have been uplifted in two stages. The first stage from 120 to 80 Ma, coincided with rifting along the eastern margin and its existence is supported by thermochronological measurements. A second stage occurred at 80–10 Ma, formed the Great Escarpment, and coincided with Cenozoic volcanism. The relationship between topography, gravity anomalies, and shear wave tomographic models suggest that regional elevation is supported by temperature anomalies within the lithosphere's thermal boundary layer. Morphology and stratigraphy of the Eastern Highlands imply that these anomalies have been coupled to the base of the plate during Australia's northward motion over the last 70 Myr.
DOI Link: 10.1002/2013JB010436
ISSN: 2169-9313
Links: http://onlinelibrary.wiley.com/doi/10.1002/2013JB010436/abstract
http://hdl.handle.net/2381/38291
Version: Publisher Version
Status: Peer-reviewed
Type: Journal Article
Rights: This is an open access article under the terms of the Creative Commons Attribution License, which permits use,distribution and reproduction in any medium, provided the original work is properly cited.
Appears in Collections:Published Articles, Dept. of Geology

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