Equilibrium fluid d18O values were calculated for aqueous fluids from which the quartz precipitated. The calculated values range from 5 to 13[[perthousand]]. They suggest the involvement of a near-surface fluid just beneath the brittle-ductile transition which is depleted in 18O relative to the fluid calculated to be in equilibrium with the local metamorphic assemblage.
The geochemical evidence of penetration of fluids depleted in 18O into ductile rocks constrains models of the mechanics of fluid flow. Ductile rocks are impermeable to fluids driven solely by thermal and topographic gradients. Simple numerical experiments illustrate the need for coupling of deformation and fluid flow to allow access of meteoric water into ductile material.
Keywords stable isotopes; fluid flow; meteoric fluids; Alpine Fault mylonites; Alpine Fault; Alpine Schist; Southern Alps; deformation coupled flow; collisional orogen
New Zealand Journal of Geology and Geophysics, 1995, Vol. 38: 535-543
0028-8306/95/3804-0535 $2.50/0 (c) The Royal Society of New Zealand 1995
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