Mylonites from three widely separated localities along the Fries ductile deformation zone in the Blue Ridge province show substantial enrichments in trace and minor elements (TiO{sub 2}, P{sub 2}O{sub 5}, Zr, Y, and V) and depletions in Rb and Sr relative to the protolith. Two end-member hypotheses can explain the enrichments: one involves partitioning to and from an infiltrating fluid and assumes that all the elements were mobile. The second hypothesis assumes the high-field-strength cations were largely immobile and that their enrichment is due to large volume losses in the mylonites. Modeling indicates that Ti is immobile for fluid/rock ratios as high as 10{sup 4}, and petrographic and modal data support a volume-loss mechanism. Volume loss was accommodated by loss of SiO{sub 2} and alkalies during feldspar dissolution. Calculated fluid/rock volume ratios required to produce the observed SiO{sub 2} losses (assuming Ti mobility) range from 70 to 600. Variable enrichments in P, Zr, Y, and V are attributed to selective mobility of these elements during fluid infiltration.
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O’Hara et al. (1989) studied this question.