Deep faulting and structural reactivation beneath the southern Illinois Basin

The investigation of deep fault structure and seismogenesis within "stable" continental interiors has been hindered by the paucity of detailed subsurface information and by low levels of seismicity. Outstanding seismotectonic questions for these areas include whether pre-existing structures govern t... Description complète

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doi: 10.1016/j.precamres.2007.02.020
Auteurs:McBride, J.H.; Leetaru, H.E.; Bauer, R.A.; Tingey, B.E.; Schmidt, S.E.A.
Volume Volume Titre:Proterozoic tectonic and crustal evolution of the upper Great Lakes region, North America
Volume Authors:Holm, D.K., editor
Source:Proterozoic tectonic and crustal evolution of the upper Great Lakes region, North America, edited by D.K. Holm, D. Schneider and V.W. Chandler. Precambrian Research, 157(1-4), p.289-313. Publisher: Elsevier, Amsterdam, International. ISSN: 0301-9268
Date de publication:2007
Remarque:In English. 71 refs.; illus., incl. sects., sketch maps
Sujets:Basement; Basin analysis; Basins; Carbon sequestration; Deep-seated structures; Depth; Earthquakes; Faults; Geologic hazards; Geophysical methods; Geophysical surveys; Grabens; Natural gas; Petroleum; Reactivation; Reflection methods; Sedimentary basins; Seismic methods; Seismic risk; Seismicity; Seismotectonics; Storage; Stress fields; Surveys; Systems; Tectonics; Illinois Basin; United States; Wabash Valley
Coordonnées:N370000 N390000 W0870000 W0900000
Identificateur:2008073395
Informations sur le Copyright:GeoRef, Copyright 2020 American Geosciences Institute. Reference includes data from CAPCAS, Elsevier Scientific Publishers, Amsterdam, Netherlands
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