Ka. Foxford et al., Extensional failure and hydraulic valving at Minas da Panasqueira, Portugal: evidence from vein spatial distributions, displacements and geometries, J STRUC GEO, 22(8), 2000, pp. 1065-1086
At Panasqueira, Portugal; exceptional exposure and demonstrable vein connec
tivity allow robust characterisation of brittle/elastic failure mechanisms
in intrusive-related environments. Extensional failure was driven by cycles
of fluid injection (hydraulic valving) and vein growth under conditions wi
th lambda(v) greater than or equal to 1 and differential stress < 4T. Failu
re was episodic and produced a swarm of W-Sn-bearing quartz veins character
ised by positive volumetric strain. Worked veins consist of families of co-
planar vein-lobes linked at branch-points. Geometrically coherent vein disp
lacements constrain an elliptical anomaly (the damage zone) in which values
of extensional strain are symmetrically distributed, decreasing systematic
ally away from a centrally located maxima to zero at a tip-line loop. Vein
textures indicate rapid. episodic, vein opening, mu m- to dm-scale vein ape
rtures, spatially and temporally variable rates of vein filling and periodi
c baffling of fluid migration pathways. Although the vein swarm represents
a single vein cluster, vein thickness and spacing populations are typically
non-power law and define anomaly-scale heterogeneous strain with inhomogen
eously deformed marginal zones surrounding a homogeneously deformed high-st
rain core. Deviations from power-law behaviour were promoted by competitive
vein growth that provided mechanisms for (i) inhibiting vein nucleation an
d (ii) localising deformation onto a few evenly spaced veins. (C) 2000 Else
vier Science Ltd. All rights reserved.