Item talk:Q100055
From geokb
{
"USGS Publications Warehouse": { "schema": { "@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Summary of workshops concerning regional seismic source zones of parts of the conterminous United States, convened by the U.S. Geological Survey, 1979-1980, Golden, Colorado", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "cir898", "url": "https://pubs.usgs.gov/publication/cir898" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 4409 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/cir898", "url": "https://doi.org/10.3133/cir898" } ], "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Circular" } ], "datePublished": "1983", "dateModified": "2018-06-21", "abstract": "Workshops were convened by the U.S. Geological Survey to obtain the latest information and concepts relative to defining seismic source zones for five regions of the United States. The zones, with some modifications, have been used in preparation of new national probabilistic ground motion hazard maps by the U.S. Geological Survey. The five regions addressed are the Great Basin, the Northern Rocky Mountains, the Southern Rocky Mountains, the Central Interior, and the northeastern United States. Discussions at the workshops focussed on possible temporal and spatial variations of seismicity within the regions, latest ages of surface-fault displacements, most recent uplift or subsidence, geologic structural provinces as they relate to seismicity, and speculation on earthquake causes. Within the Great Basin region, the zones conform to areas characterized by a predominance of faults that have certain ages of latest surface displacements. In the Northern and Southern Rocky Mountain regions, zones primarily conform to distinctive structural terrane. In the Central Interior, primary emphasis was placed on an interpretation of the areal distribution of historic seismicity, although geophysical studies in the Reelfoot rift area provided data for defining zones in the New Madrid earthquake area. An interpretation of the historic seismicity also provided the basis for drawing the zones of the New England region. Estimates of earthquake maximum magnitudes and of recurrence times for these earthquakes are given for most of the zones and are based on either geologic data or opinion.", "description": "iii, 36 p.", "publisher": { "@type": "Organization", "name": "U.S. Geological Survey" }, "author": [ { "@type": "Person", "name": "Thenhaus, P. C.", "givenName": "P. C.", "familyName": "Thenhaus" }, { "@type": "Person", "name": "McKeown, F. A.", "givenName": "F. A.", "familyName": "McKeown" }, { "@type": "Person", "name": "Bucknam, R.C.", "givenName": "R.C.", "familyName": "Bucknam" }, { "@type": "Person", "name": "Ross, D. 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