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Petrology and structure of shear-controlled anatexites in migmatite

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6070271
A close spatial relationship exists between small-scale shear structures and anatexites. The shear structures appear to provide the pathways for the release of incipient anatectic melt as well as subsequent coalescing. Braid-like interconnections of melt develop into larger-scale zones of neosome which cut older migmatite. These patterns are present in the Mount Arabia migmatite, a granitic phase of the Lithonia Gneiss, which covers more than 1800 square kilometers of the Inner Piedmont of Georgia. Mapped at a scale of 1:50, selected areas of the Mount Arabia migmatite display several stages of progressive melting from incipient metatectic films parallel to gneissic bands, to arterites composed of over 30% neosome. The migmatite shows macroscopic structural heterogeneity which appears to be related to the degree of remelting. Zones of high melt proportion consist of more ductilly deformed gneiss with contorted banding, buckle folding, mafic schlieren and pods of nebulitic migmatite. Except for its lower biotite percentage, the composition of the anatectic granite is the same as the gneiss. The petrologic and structural modification history in the Mount Arabia migmatite can be reconstructed using the composite effects of partial melt segregation, restite disaggregation, re-equilibration and contrasts in structural competance.
Research Organization:
Emory Univ., Atlanta, GA (USA)
OSTI ID:
6070271
Report Number(s):
CONF-8510489-
Conference Information:
Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
Country of Publication:
United States
Language:
English