AN INVESTIGATION OF FOOTWALL MYLONITES IN THE HARCUVAR METAMORPHIC CORE COMPLEX
We collected and analyzed samples along a NE-SW (deep to shallow) transect across the footwall. Kinematic indicators suggest a top-northeast (normal) sense of shear is present throughout the range, however, syn-deformational temperatures inferred from petrographic observations of these samples vary from greenschist to mid-upper amphibolite grade without an observable spatial pattern. The degree of footwall strain is also highly variable and does not follow a spatial pattern. Rf/Phi strain measurements generally support a dominance of non-coaxial strain with some exceptions.
Taken together, these observations suggest a more complex evolution for the footwall mylonite zone than previously believed. Temperature observations imply either that Oligo-Miocene temperatures were higher then originally hypothesized or that the mylonites formed during multiple phases. If formation of the footwall mylonites was poly-phase, kinematic observations suggest that earlier phases were also extensional in nature. We speculate that the Harcuvar core complex may have begun to form much earlier than previously recognized, perhaps during the early Tertiary. A poly-phase history would also complicate attempts to understand the geometry, strain magnitude, and total displacement of the shear zone. New EBSD and 40Ar/39Ar data are anticipated to bring new constraints on the timing and tectonic significance of the Harcuvar footwall mylonites.