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• W2005491302 abstract "[1] We image the crustal architecture of the Musgrave Province with petrophysically constrained forward models of new potential field data. These models image divergent shallow-dipping crustal scale thrusts that, at depth, link with an axial zone defined by steeper, lithospheric scale transpressional shear zones. They also show that to permit a near-surface density distribution that is consistent with petrophysical and geological observations, approximately 15–20 km of crust-mantle boundary uplift is necessary beneath the axial zone. The long-term preservation of this crust-mantle boundary offset implies a change from relatively weak lithosphere to relatively strong lithosphere during the intraplate Petermann Orogeny. To explain this, we propose a model in which uplift of the axial zone of the orogen leads to local lithospheric strengthening as a result of the uplift of mantle rocks into the lower crust, coupled with long-term lithospheric cooling due to the erosion of a radioactive upper crust. Brace-Goetze lithospheric strength models suggest that these processes may have increased the integrated strength of the lithosphere by a factor of 1.4–2.8. Because of this strengthening, this system is self-limiting, and activity will cease when lithospheric strength is sufficient to resist external forces and support isostatic imbalances. A simple force-balance model demonstrates that the force required to uplift the axial zone is tectonically reasonable and that the system can subsequently withstand significant tensional forces. This example shows that crust-mantle boundary uplift coupled with reduced crustal heat production can profoundly affect the long-term strength of the continental lithosphere and may be a critical process in the tectonic stabilization of intraplate regions." @default.
• W2005491302 created "2016-06-24" @default.
• W2005491302 creator A5002821195 @default.
• W2005491302 creator A5074841156 @default.
• W2005491302 creator A5074885968 @default.
• W2005491302 creator A5089143910 @default.
• W2005491302 date "2009-12-23" @default.
• W2005491302 modified "2023-09-23" @default.
• W2005491302 title "Constrained potential field modeling of the crustal architecture of the Musgrave Province in central Australia: Evidence for lithospheric strengthening due to crust-mantle boundary uplift" @default.
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• W2005491302 cites W1938594066 @default.
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• W2005491302 cites W1967728769 @default.
• W2005491302 cites W1971905061 @default.
• W2005491302 cites W1972238906 @default.
• W2005491302 cites W1981701295 @default.
• W2005491302 cites W1981852271 @default.
• W2005491302 cites W1983222351 @default.
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• W2005491302 cites W1985807382 @default.
• W2005491302 cites W1987324653 @default.
• W2005491302 cites W1987780664 @default.
• W2005491302 cites W1989726031 @default.
• W2005491302 cites W1989757560 @default.
• W2005491302 cites W1990122789 @default.
• W2005491302 cites W1995115331 @default.
• W2005491302 cites W1995389368 @default.
• W2005491302 cites W1997219573 @default.
• W2005491302 cites W1999820193 @default.
• W2005491302 cites W2000033909 @default.
• W2005491302 cites W2000743231 @default.
• W2005491302 cites W2004293503 @default.
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• W2005491302 cites W2010669813 @default.
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• W2005491302 cites W2011849025 @default.
• W2005491302 cites W2012675971 @default.
• W2005491302 cites W2016844673 @default.
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• W2005491302 cites W2022714845 @default.
• W2005491302 cites W2029050304 @default.
• W2005491302 cites W2029694479 @default.
• W2005491302 cites W2031089091 @default.
• W2005491302 cites W2038288419 @default.
• W2005491302 cites W2048030497 @default.
• W2005491302 cites W2049907126 @default.
• W2005491302 cites W2054654291 @default.
• W2005491302 cites W2058000463 @default.
• W2005491302 cites W2061401188 @default.
• W2005491302 cites W2062031155 @default.
• W2005491302 cites W2064025709 @default.
• W2005491302 cites W2064359381 @default.
• W2005491302 cites W2072463638 @default.
• W2005491302 cites W2075119024 @default.
• W2005491302 cites W2078813639 @default.
• W2005491302 cites W2081857714 @default.
• W2005491302 cites W2082935157 @default.
• W2005491302 cites W2083882926 @default.
• W2005491302 cites W2087570510 @default.
• W2005491302 cites W2091326991 @default.
• W2005491302 cites W2092352873 @default.
• W2005491302 cites W2093611943 @default.
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• W2005491302 cites W2096682952 @default.
• W2005491302 cites W2101339191 @default.
• W2005491302 cites W2106968845 @default.
• W2005491302 cites W2120988540 @default.
• W2005491302 cites W2122917282 @default.
• W2005491302 cites W2126094622 @default.
• W2005491302 cites W2131947476 @default.
• W2005491302 cites W2144542802 @default.
• W2005491302 cites W2148674466 @default.
• W2005491302 cites W2151971477 @default.
• W2005491302 cites W2153263119 @default.
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• W2005491302 cites W2160376258 @default.
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• W2005491302 cites W2166181258 @default.
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• W2005491302 doi "https://doi.org/10.1029/2008jb006194" @default.
• W2005491302 hasPublicationYear "2009" @default.
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