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"name": "Neotectonic and paleoseismic analysis of the northwest extent of Holocene surface deformation along the Meers Fault, Oklahoma",
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"name": "Bulletin of the Seismological Society of America",
"volumeNumber": "110",
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"abstract": "TheMeers fault (Oklahoma) is one of fewseismogenic structures with evidence for Holocene\nsurface rupture in the stable continental region of North America. The 37-kilometer-long\nsoutheast section of the full 54-kilometer-long Meers fault is interpreted to be Holocene\nactive. The 17-kilometer-long northwest section is considered Quaternary active, but not\nHolocene active.We reevaluate surface expression and earthquake timing of the northwest\nMeers fault to improve seismic source characterization.We use airborne light detection and\nranging and historical stereopaired aerial photos to evaluate the fault scarp and local faultzone\ngeomorphology. In the northwest, complex surface deformation includes fault splays,\nsubtle monoclinal warping, and a minor change in fault strike. We interpret that the alongstrike\ntransition from surface faulting on the southeastMeers fault to surface folding on the\nnorthwest Meers fault occurs at the lithologic contact between Permian Post Oak conglomerate\nand Hennessey shale. We excavated a paleoseismic trench to evaluate the timing\nof surface-deforming earthquakes on the northwest section of the fault. The excavation\nrevealed weathered Permian Hennessey shale and an \u223c1\u20132-meter-thick veneer of Holocene\nalluvial deposits that were progressively deformed during two surface-folding earthquakes\nlikely related to blind fault rupture beneath the site. Repeated onlapping to overlapping\nstratigraphic sequences and associated unconformities are intimately related to folding\nevents along the monocline. OxCal paleoearthquake age modeling indicates that earthquakes\noccurred 4704\u20133109 yr B.P. and 5955\u20134744 yr B.P., and that part of the northwest\nsection of the Meers fault is Holocene active. We find the Holocene-active section of the\nMeers fault should be lengthened 6.1 km to the northwest, to a total Holocene-active fault\nlength of 43 km. Empirical scaling relationships between surface rupture length and magnitude\nreveal that the fault could generate an Mw 7.0 earthquake.",
"description": "18 p.",
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"name": "Seismological Society of America"
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"name": "Mahan, Shannon A. smahan@usgs.gov",
"givenName": "Shannon A.",
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"name": "Hornsby, Kristofer T.",
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