FLUID FLUX GRADIENTS DURING METAMORPHISM: THE RESULT OF EXTREME CHANNELIZATION?
The veins range in width from cm to dm scale and are surrounded by chemically-altered selvages. Kyanite crystal length increases toward veins, reaching several cm in veins and selvages. Al, Fe, Mn, Zn, Li, HREE, and Y were gained in the selvages. Al was taken up by growth of kyanite, staurolite, and garnet; Fe, Mn, HREE, and Y were taken up by garnet; and Fe, Zn, and Li were taken up by staurolite. Silica was lost to the veins. Destruction of mica resulted in losses of K, Ba, Pb, and volatiles. Na and Sr losses were more variable but correlate with feldspar destruction. The selvage metasomatism and the deposition of silica and kyanite in the veins indicate that the veins were conduits for large time-integrated fluid fluxes of 2–6x104 m3 m-2 at the outcrop scale.
Numerical models of flow in fractured porous media show that fluxes can vary by orders of magnitude over distances of a meter or less adjacent to veins. High-permeability vein conduits can carry the bulk of the regional fluid flow. The lowest fluxes are expected just outside selvage margins, as most of the fluid flow is diverted into the adjacent vein-selvage zones. Thus, different workers can come to vastly different conclusions about the magnitude of fluid fluxes depending on what part of a fractured outcrop they are working in. Determining “average” time-integrated fluid fluxes across outcrops remains as an important research challenge due to the extreme spatial variability of flow.