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Journal of the Geological Society

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The nappe rule: why does it work?

^{1 1}Department of Geological Sciences, Canterbury University, Christchurch, New Zealand (e-mail: uwe.ring{at}canterbury.ac.nz)
^{2 2}Geology Department, National Research Center, 12622 Dokki, Giza, Egypt

The nappe rule stresses that imbrication emplaces nappes with higher metamorphic grade above those with lower grade. This means that the overriding nappes must be exhuming during nappe stacking; otherwise metamorphic grade would increase structurally downwards. The high-grade metamorphic internides of many orogens are characterized by a pervasive nappe-emplacement-related subhorizontal foliation indicative of vertical ductile shortening (thinning). By quantifying finite strain in the Gran Paradiso Massif, Italian Alps, we show that vertical ductile thinning associated with a nappe-emplacement-related subhorizontal foliation caused sufficient exhumation of the overriding nappes and can thus explain the occurrence of higher-grade rocks above lower-grade ones.

This article has been cited by other articles:

				U. RING and C. KUMERICS Vertical ductile thinning and its contribution to the exhumation of high-pressure rocks: the Cycladic blueschist unit in the Aegean Journal of the Geological Society, December 1, 2008; 165(6): 1019 - 1030. [Abstract] [Full Text] [PDF]