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• W2956753861 abstract "Recent earthquakes involving complex multi-fault rupture have increased our appreciation of the variety of rupture geometries and fault interactions that occur within the short duration of coseismic slip. Geometrical complexities are intrinsically linked with spatially heterogeneous slip and stress drop distributions, and hence need incorporating into seismic hazard analysis. Studies of exhumed ancient fault zones facilitate investigation of rupture processes in the context of lithology and structure at seismogenic depths. In the Gairloch Shear Zone, NW Scotland, foliated amphibolites host pseudotachylytes that record rupture geometries of ancient low-magnitude (≤MW 3) seismicity. Pseudotachylyte faults are commonly foliation parallel, indicating exploitation of foliation planes as weak interfaces for seismic rupture. Discordance and complexity are introduced by fault segmentation, stepovers, branching and brecciated dilational volumes. Pseudotachylyte geometries indicate that slip nucleation initiated simultaneously across several parallel foliation planes with millimetre and centimetre separations, leading to progressive interaction and ultimately linkage of adjacent segments and branches within a single earthquake. Interacting with this structural control, a lithological influence of abundant low disequilibrium melting-point amphibole facilitated coseismic melting, with relatively high coseismic melt pressure encouraging transient dilational sites. These faults elucidate controls and processes that may upscale to large active fault zones hosting major earthquake activity. Supplementary material: Supplementary Figures 1 and 2, unannotated versions of field photographs displayed in Figures 4a and 5 respectively, are available at https://doi.org/10.6084/m9.figshare.c.4573256 Thematic collection: This article is part of the SJG Collection on Early-Career Research available at: https://www.lyellcollection.org/cc/SJG-early-career-research" @default.
• W2956753861 created "2019-07-23" @default.
• W2956753861 creator A5012983085 @default.
• W2956753861 creator A5047910185 @default.
• W2956753861 creator A5054035527 @default.
• W2956753861 creator A5065228543 @default.
• W2956753861 date "2019-08-23" @default.
• W2956753861 modified "2023-10-16" @default.
• W2956753861 title "Rupture geometries in anisotropic amphibolite recorded by pseudotachylytes in the Gairloch Shear Zone, NW Scotland" @default.
• W2956753861 cites W1574992192 @default.
• W2956753861 cites W1830358639 @default.
• W2956753861 cites W1964733022 @default.
• W2956753861 cites W1965840332 @default.
• W2956753861 cites W1967665556 @default.
• W2956753861 cites W1968732048 @default.
• W2956753861 cites W1973893248 @default.
• W2956753861 cites W1974837455 @default.
• W2956753861 cites W1978534444 @default.
• W2956753861 cites W1980824982 @default.
• W2956753861 cites W1984546091 @default.
• W2956753861 cites W1988818557 @default.
• W2956753861 cites W1990949866 @default.
• W2956753861 cites W1992886683 @default.
• W2956753861 cites W1999329295 @default.
• W2956753861 cites W1999662231 @default.
• W2956753861 cites W2000186984 @default.
• W2956753861 cites W2000876428 @default.
• W2956753861 cites W2001835125 @default.
• W2956753861 cites W2005264158 @default.
• W2956753861 cites W2007381326 @default.
• W2956753861 cites W2008995380 @default.
• W2956753861 cites W2012734695 @default.
• W2956753861 cites W2015393038 @default.
• W2956753861 cites W2017625755 @default.
• W2956753861 cites W2020017204 @default.
• W2956753861 cites W2024618100 @default.
• W2956753861 cites W2024861829 @default.
• W2956753861 cites W2028956463 @default.
• W2956753861 cites W2037646551 @default.
• W2956753861 cites W2042520007 @default.
• W2956753861 cites W2046954417 @default.
• W2956753861 cites W2048915930 @default.
• W2956753861 cites W2050089827 @default.
• W2956753861 cites W2051890541 @default.
• W2956753861 cites W2053601733 @default.
• W2956753861 cites W2053812342 @default.
• W2956753861 cites W2059108815 @default.
• W2956753861 cites W2060336025 @default.
• W2956753861 cites W2061976920 @default.
• W2956753861 cites W2067232314 @default.
• W2956753861 cites W2069419430 @default.
• W2956753861 cites W2074070400 @default.
• W2956753861 cites W2076190086 @default.
• W2956753861 cites W2077712098 @default.
• W2956753861 cites W2078575244 @default.
• W2956753861 cites W2081032963 @default.
• W2956753861 cites W2090460564 @default.
• W2956753861 cites W2092035410 @default.
• W2956753861 cites W2093820542 @default.
• W2956753861 cites W2096105657 @default.
• W2956753861 cites W2096347223 @default.
• W2956753861 cites W2096459584 @default.
• W2956753861 cites W2108351382 @default.
• W2956753861 cites W2109176436 @default.
• W2956753861 cites W2116783659 @default.
• W2956753861 cites W2117221055 @default.
• W2956753861 cites W2120007352 @default.
• W2956753861 cites W2130177394 @default.
• W2956753861 cites W2132755246 @default.
• W2956753861 cites W2133580092 @default.
• W2956753861 cites W2147474159 @default.
• W2956753861 cites W2148872613 @default.
• W2956753861 cites W2149808122 @default.
• W2956753861 cites W2156245371 @default.
• W2956753861 cites W2161503203 @default.
• W2956753861 cites W2163308577 @default.
• W2956753861 cites W2164683099 @default.
• W2956753861 cites W2165149348 @default.
• W2956753861 cites W2170076374 @default.
• W2956753861 cites W2256660466 @default.
• W2956753861 cites W2269732048 @default.
• W2956753861 cites W2274228398 @default.
• W2956753861 cites W2320500117 @default.
• W2956753861 cites W2328040794 @default.
• W2956753861 cites W2536711694 @default.
• W2956753861 cites W2597795855 @default.
• W2956753861 cites W2607789580 @default.
• W2956753861 cites W2767359585 @default.
• W2956753861 cites W2773374934 @default.
• W2956753861 cites W2792688520 @default.
• W2956753861 cites W2807276036 @default.
• W2956753861 cites W2884903314 @default.
• W2956753861 cites W2889136619 @default.
• W2956753861 cites W2890617922 @default.
• W2956753861 cites W2945642044 @default.
• W2956753861 cites W648083478 @default.
• W2956753861 doi "https://doi.org/10.1144/sjg2019-003" @default.
• W2956753861 hasPublicationYear "2019" @default.

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