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Geological Society, London, Special Publications; 1990; v. 54; p. 167-173;
DOI: 10.1144/GSL.SP.1990.054.01.16
© 1990 Geological Society of London

Instabilities and Localization

Reaction-enhanced formation of eclogite-facies shear zones in granulite-facies anorthosites

Eva M. Klaper

Institute of Geology, Bern University, Baltzerstr. 1, 3012 Bern, Switzerland

Infiltration of a dry granulite-facies anorthosite complex by a hydrous fluid phase under high pressure was crucial to start (a) an eclogitization process which led to the breakdown of plagioclase and the formation of either dense or hydrated minerals and (b) dynamic recrystallization of plagioclase in shear zones. Reaction products of the eclogitization process are related spatially to cracks and shear zones. The reduction in grain size during dynamic recrystallization, the foliation development in shear zones and the occurrence of new ‘soft’ and/or dense minerals changed the mechanical properties (e.g. ductility) of the rocks considerably.

The initiation of detachment and thrusting in the lower crust may be an important large scale consequence of such localized processes.





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