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Neotectonics and Quaternary Fault-reactivation in Europe's Intraplate Lithosphere

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Pronounced lateral variations in Europe's intraplate strength occur, as a result of thermal perturbation in the underlying mantle and inherited inhomogeneity in lithospheric structures, as a result of Europe's polyphase pre-Quaternary evolution. This book presents the results from quantitative subsidence analysis studies.

280 pages, Hardcover

First published August 4, 2005

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