2013
DOI: 10.1007/s00531-013-0875-7
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Long-lived crustal-scale fluid flow: the hydrothermal mega-breccia of Hidden Valley, Mt. Painter Inlier, South Australia

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Cited by 27 publications
(28 citation statements)
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“…For simplicity we consider the mineral reaction biotite → feldspar + Fe/Mg-oxide + water as the single fluid source, which has been suggested for the Mount Painter breccias [4]. We further assume that the reaction occurs at a depth of 16 km depth [e.g., 4,50].…”
Section: Fluid Flow and Hydraulic Fracturing In The Earth's Crustmentioning
confidence: 99%
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“…For simplicity we consider the mineral reaction biotite → feldspar + Fe/Mg-oxide + water as the single fluid source, which has been suggested for the Mount Painter breccias [4]. We further assume that the reaction occurs at a depth of 16 km depth [e.g., 4,50].…”
Section: Fluid Flow and Hydraulic Fracturing In The Earth's Crustmentioning
confidence: 99%
“…Veins are dilatant structures, typically fractures, filled with minerals that precipitated from fluid (see review of [1], and references therein). Hydraulic breccias are fragmented rocks where the fragmentation is mainly caused by chaotic fracturing due to fluid overpressure [2][3][4][5], as opposed to tectonic breccias where the diminution is due to tectonic stresses, typically along faults [6][7][8].…”
Section: Introductionmentioning
confidence: 99%
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