Journal of Petrology | Volume 37 | Number 2 | Pages 395-414 | 1996
© Oxford University Press 1996
research-article |
Metapelitic Migmatites from Brattstrand Bluffs, East AntarcticaMetamorphism, Melting and Exhumation of the Mid Crust
DEPARTMENT OF GEOLOGY AND GEOPHYSICS, UNIVERSITY OF EDINBURGH, THE GRANT INSTITUTE WEST MAINS ROAD, EDINBURGH EH9 SJW, UK
Received August 22, 1995; Revised typescript accepted November 6, 1995
ABSTRACT
Metapelitic migmatites at Brattstrand Bluffs, East Antarctica, preserve granulite assemblages and a complex deformational history. Crystallized granitic melt accounts for
25% of exposed rocks, and was produced by biotite dehydration-melting reactions in the host metapelite. Variable degrees of melt production and extraction resulted in a range of bulk compositions in the residual metapelite, from quartz-rich migmatites to restitic quartz-absent pelite. Decompressional reaction textures indicate
11 km of exhumation after peak metamorphism at PT conditions of
6 kbar and
860°C Decompression occurred during a single cycle of partial melting and melt crystallization at
500 Ma, and was synchronous with tectonic unroofing of the Brattstrand Bluffs migmatites along ductile shear zones. Exhumation has been proposed as a cause of dehydration melting in the Himalaya and elsewhere, but melting at Brattstrand Bluffs was ultimately driven by the tectonic perturbation and subsequent thermal relaxation responsible for high metamorphic temperatures. Exhumation did not drive melting reactions, but it is likely that the presence of melt focused deformation in the migmatites and thus promoted exhumation.
KEY WORDS: decompression; exhumation; granulite; melting; migmalite
*Corresponding author.
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