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Optimally oriented ‘‘fault-valve’’ thrusts : evidence for aftershock-related fluid pressure pulses?
Micklethwaite, S (2008) Optimally oriented ‘‘fault-valve’’ thrusts : evidence for aftershock-related fluid pressure pulses? Geochemistry, Geophysics, Geosystems, 9 (4). pp. 1-10.
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A thrust-vein network from the Triumph gold deposit, Western Australia, is explained in terms of an
extremely high rate of fluid-pressure increase, prior to failure, relative to the rate of stress increase. The
thrust fault is a small-displacement fault characterized by a thick, fault-parallel shear vein, plus multiple
low-angle extension veins, with orientations that demonstrate the thrust was optimally oriented relative to
the locally imposed crustal stresses. Large extension veins have irregular margins, are dominantly
composed of coarse milky quartz with no obvious laminations or solid inclusion trails, and are regularly
spaced along the thrust (1–2 m). The fault-vein geometries indicate the Triumph thrust is a rare candidate
for ‘‘fault-valve’’ failure of an optimally oriented thrust, and it is possible the structure formed in a small
number of failure events, during load weakening of the thrust. An analysis using the Coulomb criterion
shows that load weakening of a thrust occurs when fluid pressure increases relative to tectonic stress by a
factor dependent on the orientation of the thrust. Thrust and reverse faults in dry crust load strengthen prior
to failure, but the poroelastic behavior of sealed, fluid-saturated crust is enough to induce load weakening
in compressive environments; thus poroelastic load weakening is expected to be an important failure
mechanism in hydrothermal environments. However, in the case of the Triumph thrust, dilatant shear
failure necessitates a fluid pressure increase which is an order of magnitude larger still. The observations
and results are consistent with a pulse of high fluid pressure migrating up through fault or fracture
networks that have elevated permeability relative to the wall rock, under conditions of transiently low
differential stress. Fluid pressure differences resulted between the fault and wall rock, leading to extension
fracture and fault failure. Such conditions may occur when adjacent large earthquakes induce damage,
breach overpressured fluid reservoirs, and generate fluid-pressure driven aftershocks.
|Keywords:||fluid pressure; load weakening; veins; thrust; aftershocks; mineral deposit|
|Journal or Publication Title:||Geochemistry, Geophysics, Geosystems|
|Page Range:||pp. 1-10|
|Identification Number - DOI:||10.1029/2007GC001916|
Copyright 2008 by the American Geophysical Union.
|Date Deposited:||24 Nov 2008 23:31|
|Last Modified:||18 Nov 2014 03:53|
|Item Statistics:||View statistics for this item|
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