Item talk:Q240184
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "A fault\u2010based model for crustal deformation in the western United States based on a combined inversion of GPS and geologic inputs", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70191363", "url": "https://pubs.usgs.gov/publication/70191363" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70191363 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1785/0120150362", "url": "https://doi.org/10.1785/0120150362" } ], "journal": { "@type": "Periodical", "name": "Bulletin of the Seismological Society of America", "volumeNumber": "107", "issueNumber": "6" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Bulletin of the Seismological Society of America" } ], "datePublished": "2017", "dateModified": "2018-03-28", "abstract": "We develop a crustal deformation model to determine fault\u2010slip rates for the western United States (WUS) using the\u00a0Zeng and Shen (2014)\u00a0method that is based on a combined inversion of Global Positioning System (GPS) velocities and geological slip\u2010rate constraints. The model consists of six blocks with boundaries aligned along major faults in California and the Cascadia subduction zone, which are represented as buried dislocations in the Earth. Faults distributed within blocks have their geometrical structure and locking depths specified by the Uniform California Earthquake Rupture Forecast, version 3 (UCERF3) and the 2008 U.S. Geological Survey National Seismic Hazard Map Project model. Faults slip beneath a predefined locking depth, except for a few segments where shallow creep is allowed. The slip rates are estimated using a least\u2010squares inversion. The model resolution analysis shows that the resulting model is influenced heavily by geologic input, which fits the UCERF3 geologic bounds on California B faults and \u00b1one\u2010half of the geologic slip rates for most other WUS faults. The modeled slip rates for the WUS faults are consistent with the observed GPS velocity field. Our fit to these velocities is measured in terms of a normalized chi\u2010square, which is 6.5. This updated model fits the data better than most other geodetic\u2010based inversion models. Major discrepancies between well\u2010resolved GPS inversion rates and geologic\u2010consensus rates occur along some of the northern California A faults, the Mojave to San Bernardino segments of the San Andreas fault, the western Garlock fault, the southern segment of the Wasatch fault, and other faults. Off\u2010fault strain\u2010rate distributions are consistent with regional tectonics, with a total off\u2010fault moment rate of\u00a07.2\u00d71018\u00a0and\u00a08.5\u00d71018\u2009\u2009N\u22c5m/year\u00a0for California and the WUS outside California, respectively.", "description": "16 p.", "publisher": { "@type": "Organization", "name": "Seismological Society of America" }, "author": [ { "@type": "Person", "name": "Zeng, Yuehua zeng@usgs.gov", "givenName": "Yuehua", "familyName": "Zeng", "email": "zeng@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0003-1161-1264", "url": "https://orcid.org/0000-0003-1161-1264" }, "affiliation": [ { "@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center" } ] }, { "@type": "Person", "name": "Shen, Zheng-Kang", "givenName": "Zheng-Kang", "familyName": "Shen" } ], "funder": [ { "@type": "Organization", "name": "Geologic Hazards 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