1. The Fluid Rock Interaction Group, Departments of Geology & Physics, University of Oslo, PO Box 1047 Blindern, N-0316 Oslo , Norway

Correspondence to: Bjørn Jamtveit Correspondence and requests for materials should be addressed to B.J. (e-mail: Email: bjorn.jamtveit@geologi.uio.no).

Abstract

The metamorphic cycle associated with the formation of mountain belts produces a lower crust containing little or no free fluid^{1, 2}. The introduction of external fluids to dry and impermeable volumes of the Earth's crust is thus a prerequisite for the retrogressive metamorphism later observed in such regimes. Such metamorphism can cause significant changes in the crust's physical properties, including its density, rheology and elastic properties^{3, 4}. On a large scale, the introduction of fluids requires the presence of high-permeability channels, such as faults or fractures, which are the result of external tectonic stresses. But extensive interaction between externally derived fluids and the fractured rock requires efficient mass transport away from the initial fractures into the rock itself, and this transport often occurs over distances much longer than expected from grain-boundary diffusion. Here we present both field observations and a simple network model that demonstrate how the transport of fluids into initially dry rock can be accelerated by perturbations in the local stress field caused by reactions with fluids. We also show that the morphology of reaction fronts separating 'dry' from 'wet' rocks depends on the anisotropy of the external stress field.