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• W2021138049 abstract "Strain heating results from the conversion of mechanical energy into heat during progressive deformation. As a physical phenomenon it is well known in fluid mechanics and has been studied theoretically and experimentally. This work has been extended by recent geophysical developments. Here we review (a) the fluid mechanics and geophysical work and (b) its application to continental shear zones. The models indicate that temperature rises of a few hundred degrees can be expected in major shear zones (transcurrent shear zones, the bases of thrust sheets, or the margins of large diapirs). In certain special situations (some thrust sheets and nappes), even larger rises are possible. The resulting temperature gradients should be detectable geologically, but evidence is scanty. The resulting thermal softening is sufficient to concentrate most of the deformation in narrow zones. Thus strain heating is an important crustal phenomenon which should be incorporated in models of large-scale tectonic processes. It may even contribute to local partial melting in some shear zones." @default.
• W2021138049 created "2016-06-24" @default.
• W2021138049 creator A5014690995 @default.
• W2021138049 creator A5019165446 @default.
• W2021138049 date "1980-01-01" @default.
• W2021138049 modified "2023-09-26" @default.
• W2021138049 title "Strain heating and thermal softening in continental shear zones: a review" @default.
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• W2021138049 doi "https://doi.org/10.1016/0191-8141(80)90045-0" @default.
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