By C. A. J. Wibberley, W. Kurz, J. Imber, R. E. Holdsworth, C. Collettini
Faults are basic focuses of either fluid migration and deformation within the top crust. the popularity that faults tend to be heterogeneous zones of deformed fabric, no longer easy discrete fractures, has basic implications for a way geoscientists expect fluid migration in fault zones, in addition to resulting in new recommendations in knowing seismic/aseismic pressure lodging. This publication captures present learn into realizing the complexities of fault-zone inner constitution, and their regulate on mechanical and fluid-flow homes of the higher crust. a wide selection of techniques are offered, from geological box reviews and laboratory analyses of fault-zone and fault-rock homes to numerical fluid-flow modelling, and from seismological information analyses to coupled hydraulic and rheological modelling. The ebook goals to demonstrate the significance of figuring out fault-zone complexity by means of integrating such assorted techniques, and its effect at the rheological and fluid-flow behaviour of fault zones in numerous contexts.Also available:The dating among harm and Localization - ISBN 978-1-86239-236-6Rock Physics and Geomechanics within the learn of Reservoirs and Repositories - ISBN 978-1-86239-230-4Analogue and Numerical Modelling of Crustal-Scale approaches - ISBN 978-1-86239-191-8The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on the earth, and one of many greatest publishers within the Earth sciences.The Society publishes a variety of fine quality peer-reviewed titles for lecturers and execs operating within the geosciences, and enjoys an enviable foreign recognition for the standard of its work.The many parts during which we submit in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic reports and geochemistry-Remote sensing-History of geology-Regional geology courses
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Extra resources for The Internal Structure of Fault Zones: Implications for Mechanical and Fluid-Flow Properties (Geological Society Special Publication No. 299)
Sample text
E. & C OLLETTINI , C. (eds) The Internal Structure of Fault Zones. Geological Society, London, Special Publications, 299, 75–95. B ROWN , A. 2003. Capillary effects on fault-fill sealing. American Association of Petroleum Geologists Bulletin, 87, 381– 395. B RUHN , R. , P ARRY , W. , Y ONKEE , W. A. & T HOMPSON , T. 1994. Fracturing and hydrothermal alteration in normal fault zones. Pure and Applied Geophysics, 142, 609– 644. B UTLER , C. , H OLDSWORTH , R. E. & S TRACHAN , R. A. 1995. Evidence for Caledonian sinistral strikeslip motion and associated fault zone weakening, Outer Hebrides Fault Zone, Scotland.
G IBSON , R. G. 1994. Fault-zone seals in siliclastic strata of the Columbus Basin, offshore Trinidad. AAPG Bulletin, 78, 1372–1385. G IBSON , R. G. 1998. Physical character and fluidflow properties of sandstone-derived fault gouge. In: C OWARD , M. , D ALTABAN , T. S. & J OHNSON , H. (eds) Structural Geology in Reservoir Characterzation. Geological Society, London, Special Publications, 127, 83– 97. G IBSON , R. G. & B ENTHAM , P. A. 2003. Use of fault-seal analysis in understanding petroleum migration in a complexly faulted anticlinal trap, Columbus Basin, offshore Trinidad.
D IETERICH , J. H. 1979. Modeling of rock friction 1. Experimental results and constitutive equations, Journal of Geophysical Research, 84, 2161–2168. D I T ORO , G. & P ENNACCHIONI , G. 2005. Fault plane processes and mesoscopic structure of a strong-type seismogenic fault in tonalites (Adamello batholith, Southern Alps). Tectonophysics, 402, 54–79. , G OLDSBY , D. L. & T ULLIS , T. E. 2004. Friction falls towards zero in quartz rock as slip velocity approaches seismic rates. Nature, 427, 436–439.
