Item talk:Q242812
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Late quaternary slip-rate variations along the Warm Springs Valley fault system, northern Walker Lane, California-Nevada border", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70038472", "url": "https://pubs.usgs.gov/publication/70038472" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70038472 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1785/0120120020", "url": "https://doi.org/10.1785/0120120020" } ], "journal": { "@type": "Periodical", "name": "Bulletin of the Seismological Society of America", "volumeNumber": "103", "issueNumber": "1" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Bulletin of the Seismological Society of America" } ], "datePublished": "2013", "dateModified": "2020-09-11", "abstract": "The extent to which faults exhibit temporally varying slip rates has important consequences for models of fault mechanics and probabilistic seismic hazard. Here, we explore the temporal behavior of the dextral\u2010slip Warm Springs Valley fault system, which is part of a network of closely spaced (10\u201320 km) faults in the northern Walker Lane (California\u2013Nevada border). We develop a late Quaternary slip record for the fault using Quaternary mapping and high\u2010resolution topographic data from airborne Light Distance and Ranging (LiDAR). The faulted Fort Sage alluvial fan (40.06\u00b0 N, 119.99\u00b0 W) is dextrally displaced 98+42/-43 m, and we estimate the age of the alluvial fan to be 41.4+10.0/-4.8 to 55.7\u00b19.2\u2009\u2009ka, based on a terrestrial cosmogenic 10Be depth profile and 36Cl analyses on basalt boulders, respectively. The displacement and age constraints for the fan yield a slip rate of 1.8 +0.8/-0.8 mm/yr to 2.4 +1.2/-1.1 mm/yr (2\u03c3) along the northern Warm Springs Valley fault system for the past 41.4\u201355.7 ka. In contrast to this longer\u2010term slip rate, shorelines associated with the Sehoo highstand of Lake Lahontan (~15.8\u2009\u2009ka) adjacent to the Fort Sage fan are dextrally faulted at most 3 m, which limits a maximum post\u201015.8 ka slip rate to 0.2\u2009\u2009mm/yr. These relations indicate that the post\u2010Lahontan slip rate on the fault is only about one\u2010tenth the longer\u2010term (41\u201356 ka) average slip rate. 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