Abstract
The metamorphic cycle associated with the formation of mountain belts produces a lower crust containing little or no free fluid1,2. 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 properties3,4. 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.
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References
Yardley, B. W. D. in Fluid Flow and Transport in Rocks: Mechanisms and Effects (eds Jamtveit, B. & Yardley, B. W. D.) 99–121 (Chapman and Hall, London, 1997).
Yardley, B. W. D. & Valley, J. W. The petrologic case for a dry lower crust. J. Geophys. Res. 102, 12173–12185 (1997).
Austrheim, H. Eclogitization of lower crustal granulites by fluid migration through shear zones. Earth Planet. Sci. Lett. 81, 221– 232 (1987).
Austrheim, H. Eclogite formation and the dynamics of crustal roots under continental collision zones. Terra Nova 3, 492– 499 (1991).
Sturt, B. A., Skarpenes, O., Ohanian, A. T. & Pringle, T. R. Reconnaissance Rb/Sr isochron study in the Bergen Arc System and regional implications Nature 253, 595– 599 (1975).
Bingen, B., Davis, W. J. & Austrheim, H. Zircon growth during fluid induced Caledonian/Scandian eclogite-facies metamorphism of the Lindås Nappe, Caledonides of W Norway. Min. Mag. A 62, 161–162 (1998).
Jamtveit, B., Bucher-Nurminen, K. & Austrheim, H. Fluid controlled eclogitization of granulites in deep crustal shear zones, Bergen Arcs, western Norway. Contrib. Mineral. Petrol. 104, 184–193 ( 1990).
Rockow, K. M., Haskin, L. A., Jolliff, B. L. & Fountain, D. M. Constraints on element mobility associated with the conversion of granulite to eclogite along fractures in an anorthositic complex on Holsnoy, Norway. J. Metamorph. Geol. 15, 401– 418 (1997).
Wheeler, J. The significance of grain-scale kinetics of metamorphism. Contrib. Mineral. Petrol. 97, 397–404 (1987).
Kirkaldy, J. S. in Growth, Dissolution and Pattern Formation in Geosystems (eds Jamtveit, B. & Meakin, P.) 189–220 (Kluwer, Dordrecht, 1999).
Cundall, P. A. & Strack, O. D. L. A discrete numerical model for granular asssemblies. Geotechnique 29, 47–65 (1979)
de Arcangelis, L. & Reder, S. A random fuse model for breaking processes. J. Phys. Lett. 46, L585–L590 (1985).
Herrmann, H. J. & Roux, S. Statistical Models for the Fracture of Disordered Media. (North-Holland, Amsterdam, 1990).
Herrmann, H. J., Hansen, A. & Roux, S. Fracture of disordered, elastic lattices in two dimension. Phys. Rev. B 39, 637–648 (1989).
Malthe-Sorenssen, A. et al. Simulation of extensional clay fractures. Phys. Rev. E 58, 5548–5564 ( 1998).
Yakobson, B. I. Morphology and rate of fracture in chemical decomposition of solids. Phys. Rev. Lett. 67, 1590–1593 (1991).
Farver, J. R. & Yund, R. A. Oxygen bulk diffusion measurements and TEM characterization of a natural ultramylonite: implications for fluid transport in mica-bearing rocks. J. Metamorph. Geol. 17, 669–683 (1999).
Roark, R. J. & Young, W. C. Formulas for Stress and Strain (McGraw Hill, Tokyo, 1975).
Allen, D. M. de G. Relaxation Methods (McGraw-Hill, New York, 1954).
Acknowledgements
This work was funded by the Norwegian Research Council through a grant to the Strategic University Program ‘Fluid Rock Interactions’. We thank J. Feder, P. Meakin and the other members of the Fluid Rock Interaction group for valuable suggestions and discussions and A. Kühn and M. Lund for providing some of the figures.
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Jamtveit, B., Austrheim, H. & Malthe-Sørenssen, A. Accelerated hydration of the Earth's deep crust induced by stress perturbations . Nature 408, 75–78 (2000). https://doi.org/10.1038/35040537
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DOI: https://doi.org/10.1038/35040537
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