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- W2022086116 abstract "(50 mW m −2 ). In contrast, localized mantle deformation is most pronounced when the extended lithosphere has a normal crustal thickness (30–40 km) and an intermediate heat flow (60–70 mW m −2 ). Results show a nonlinear response to subtle changes in crustal thickness or heat flow, characterized by abrupt and sometimes unexpected switches in extension modes (e.g., from diffuse extensional deformation to effective lithospheric‐scale rupturing) or from mantle‐ to crust‐dominated strain localization. We interpret this nonlinearity to result from the interference of doming wavelengths in the presence of multiple necking instabilities. Disharmonic crust and mantle doming wavelengths results in efficient communication between shear zones at different lithospheric levels, leading to rupturing of the whole lithosphere. In contrast, harmonic crust and mantle doming inhibits interaction of shear zones across the lithosphere and results in a prolonged history of extension prior to continental breakup." @default.
- W2022086116 created "2016-06-24" @default.
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- W2022086116 date "2010-11-25" @default.
- W2022086116 modified "2023-09-23" @default.
- W2022086116 title "Interaction between mantle and crustal detachments: A nonlinear system controlling lithospheric extension" @default.
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- W2022086116 doi "https://doi.org/10.1029/2009jb006696" @default.
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