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The spin zone: Transient mid-crust permeability caused by coseismic brecciation
Institution:1. Department of Earth and Planetary Sciences, McGill University, Montréal, QC H3A 0E8, Canada;2. Department of Geological Sciences, University of Cape Town, Private Bag X3, Rondebosch 7701, South Africa;3. School of Earth and Climate Sciences, University of Maine, Orono, ME 04469, United States;1. Tohoku University, 6-6-20 Aramaki-Aza-Aoba, Aobaku, Sendai, 980-8579, Japan;2. OYO Corporation, 2-2-19 Daitakubo, Minamiku, Saitama, 336-0015, Japan;1. Laboratorio de Ingeniería de Reservorios, Instituto del Gas y del Petróleo, Facultad de Ingeniería, Universidad de Buenos Aires, Av. Las Heras 2214 Piso 3, C1127AAR Buenos Aires, Argentina;2. Instituto del Gas y del Petróleo, Facultad de Ingeniería, Universidad de Buenos Aires, CONICET, Argentina;3. Universidad de La Plata, Argentina;4. Department of Mathematics, Purdue University, 150 N. University Street, West Lafayette, IN 47907-2067, USA;5. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42c, 34010 Sgonico, Trieste, Italy;1. Research Center of Small Sample Technology, Beijing University of Aeronautics and Astronautics, Beijing 100191, China;2. Army Aviation Research Institute, Beijing 101123, China;1. CAS Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou City, 510640, China;2. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou City, 510640, China
Abstract:
Keywords:Breccia  Earthquake  Brittle-plastic transition  Fluid flow  Pofadder Shear Zone
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