Hydrogeologic controls on induced seismicity in crystalline basement rocks due to fluid injection into basal reservoirs

A series of Mb 3.8-5.5 induced seismic events in the midcontinent region, United States, resulted from injection of fluid either into a basal sedimentary reservoir with no underlying confining unit or directly into the underlying crystalline basement complex. The earthquakes probably occu... Volledige beschrijving

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doi: 10.1111/gwat.12071
Auteurs:Zhang, Y.; Person, M.; Rupp, J.; Ellett, K.; Celia, M.A.; Gable, C.W.; Bowen, B.; Evans, J.; Bandilla, K.; Mozley, P.; Dewers, T.; Elliot, T.
Volume Title:Ground Water
Bron:Ground Water, 51(4), p.525-538. Publisher: Wiley-Blackwell on behalf of National Ground Water Association, Westerville, OH, United States. ISSN: 0017-467X
Publicatiedatum:2013
Opmerking:In English. 58 refs.; illus., incl. 2 tables, geol. sketch maps
Onderwerpen:Aquifers; Basement; Boundary conditions; Carbon dioxide; Carbon sequestration; Controls; Crystalline rocks; Earthquakes; Equations; Failures; Faults; Fluid injection; Focus; Ground water; Hazardous waste; Hydrogeology; Induced earthquakes; Injection; Magdalena Group; Models; Numerical models; Oil and gas fields; Oil wells; Paleoseismicity; Paleozoic; Permeability; Pollution; Risk assessment; Three-dimensional models; Waste disposal; Water wells; Waterflooding; Arkansas; Illinois; Illinois Basin; Indiana; Midwest; Ohio; United States; Enders Fault; Ozark Aquifer
Coördinaten:N310000 N430000 W0780000 W0950000
Record ID:2013084802
Copyright Information:GeoRef, Copyright 2020 American Geosciences Institute. Reference includes data from John Wiley & Sons, Chichester, United Kingdom
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