Definition and Introduction
The continental lithosphere consists of the continental crust and, typically, some nonconvecting part of the underlying upper mantle (Fig. 1). In plate tectonics terms, the continental lithosphere is part of the rigid outer rind of the Earth, which is segmented into several major plates. The cold lithosphere lies atop a hotter, more mobile (low strength) asthenosphere. In this context, oceanic lithosphere for the most part obeys comparatively simple thermal models, with the boundary between lithosphere and asthenosphere represented by an isotherm marking the transition in mantle peridotite between elastic and ductile behavior (but see “Lithosphere, Oceanic”for the growing list of complications). By contrast, the continental lithosphere is heterogeneous and its structure highly variable. That contrast reflects the fact that oceanic lithosphere is formed in much the same way worldwide and that it is continually recycled into the interior of the Earth via the...
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James, D.E. (2020). Lithosphere, Continental. In: Gupta, H. (eds) Encyclopedia of Solid Earth Geophysics. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-030-10475-7_32-1
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