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• W2038202477 endingPage "1136" @default.
• W2038202477 startingPage "1127" @default.
• W2038202477 abstract "The mesozonal environment for mineralisation (∼10±5 km depth) occurs towards the base of the seismogenic zone in the upper continental crust which, in areas of strong fluid release, acts as a stressed elastic lid containing overpressured hydrothermal fluids derived from metamorphic dehydration at depth. Au–quartz lodes in this environment are hosted by fault–fracture meshes comprising dilatant extensional and extensional-shear fractures interlinked by low-displacement faults. They form in a range of tectonic regimes but are most extensively developed in compressional/transpressional settings. A brittle failure mode plot contrasting compressional and extensional stress regimes demonstrates that: (i) high fluid overpressures are easier to sustain in compressional regimes that also allow the highest amplitude fluid-pressure cycling; (ii) dilatant mesh structures serve as high-permeability conduits only under high fluid-pressure and low differential stress in the absence of through-going cohesionless faults that are well-oriented for reactivation; and, (iii) the critical interdependence of differential stress and sustainable overpressure ensures that changes in stress state are accompanied by fluid redistribution. The specialised circumstances allowing high-flux flow of overpressured fluids are generally short-lived and are terminated by the formation of through-going, favourably oriented faults." @default.
• W2038202477 created "2016-06-24" @default.
• W2038202477 creator A5043712271 @default.
• W2038202477 date "2004-06-01" @default.
• W2038202477 modified "2023-10-06" @default.
• W2038202477 title "Controls on maximum fluid overpressure defining conditions for mesozonal mineralisation" @default.
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• W2038202477 doi "https://doi.org/10.1016/j.jsg.2003.11.003" @default.
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