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Titlebook: Basement Tectonics 11 Europe and Other Regions; Proceedings of the E O. Oncken,C. Janssen Conference proceedings 1996 Springer Science+Busi

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Hegel—From Foundation to Systemquired us to develop a solution to each it these problem areas; therefore the key section not only represents a summary of the available data but also an interpretation of the deep crustal tectonics of the northern Apennines.
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Lower Continental Crust Exhumed: Granulite Grade Terranes and Amphibolite Grade Shear Zones in the Aramafic compositions (Percival et al., 1992, Rutter and Brodie, 1992 and Zingg et al., 1990). Dates from the lower crustal rocks are “very poorly constrained” (Downes, 1993). This paper discusses the isotopically dated two-stages of lower crust formation and the absence of the upper crust in the Anabar shield.
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Late-Orogenic Burial and Exhumation at a Major Variscan Suture Zonea and subsequently slowed down to 20 mm/a. Exhumation in the direct vicinity of the suture zone occurred temporarily at velocities of more than 3 mm/a. Such rapid decompression strongly suggests a significant contribution of extensional strain to the Late Variscan exhumation of the study area.
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