Item talk:Q306202

{

 "USGS Publications Warehouse": {
   "@context": "https://schema.org",
   "@type": "Article",
   "additionalType": "Journal Article",
   "name": "The Wasatch fault zone, utah-segmentation and history of Holocene earthquakes",
   "identifier": [
     {
       "@type": "PropertyValue",
       "propertyID": "USGS Publications Warehouse IndexID",
       "value": "70016367",
       "url": "https://pubs.usgs.gov/publication/70016367"
     },
     {
       "@type": "PropertyValue",
       "propertyID": "USGS Publications Warehouse Internal ID",
       "value": 70016367
     },
     {
       "@type": "PropertyValue",
       "propertyID": "DOI",
       "value": "10.1016/0191-8141(91)90062-N",
       "url": "https://doi.org/10.1016/0191-8141(91)90062-N"
     },
     {
       "@type": "PropertyValue",
       "propertyID": "ISSN",
       "value": "01918141"
     }
   ],
   "journal": {
     "@type": "Periodical",
     "name": "Journal of Structural Geology",
     "volumeNumber": "13",
     "issueNumber": "2"
   },
   "inLanguage": "en",
   "isPartOf": [
     {
       "@type": "CreativeWorkSeries",
       "name": "Journal of Structural Geology"
     }
   ],
   "datePublished": "1991",
   "dateModified": "2024-05-10",
   "abstract": "The Wasatch fault zone (WFZ) forms the eastern boundary of the Basin and Range province and is the longest continuous, active normal fault (343 km) in the United States. It underlies an urban corridor of 1.6 million people (80% of Utah's population) representing the largest earthquake risk in the interior of the western United States.We have used paleoseismological data to identify 10 discrete segments of the WFZ. Five are active, medial segments with Holocene slip rates of 1\u20132 mm a\u22121, recurrence intervals of 2000\u20134000 years and average lengths of about 50 km. Five are less active, distal segments with mostly pre-Holocene surface ruptures, late Quaternary slip rates of <0.5 mm a\u22121\u00a0recurrence intervals of \u226510,000 years and average lengths of about 20 km. Surface-faulting events on each of the medial segments of the WFZ formed 2\u20134-m-high scarps repeatedly during the Holocene; latest Pleistocene (14\u201315 ka) deposits commonly have scarps as much as 15\u201320 m in height. Segments identified from paleoseismological studies of other major late Quaternary normal faults in the northern Basin and Range province are 20\u201325 km long, or about half of that proposed for the medial segments of the WFZ.",
   "description": "13 p.",
   "publisher": {
     "@type": "Organization",
     "name": "Elsevier"
   },
   "author": [
     {
       "@type": "Person",
       "name": "Machette, M. N.",
       "givenName": "M. N.",
       "familyName": "Machette"
     },
     {
       "@type": "Person",
       "name": "Personius, S. F.",
       "givenName": "S. F.",
       "familyName": "Personius",
       "identifier": {
         "@type": "PropertyValue",
         "propertyID": "ORCID",
         "value": "0000-0001-8347-7370",
         "url": "https://orcid.org/0000-0001-8347-7370"
       }
     },
     {
       "@type": "Person",
       "name": "Schwartz, D. P.",
       "givenName": "D. P.",
       "familyName": "Schwartz",
       "identifier": {
         "@type": "PropertyValue",
         "propertyID": "ORCID",
         "value": "0000-0001-5193-9200",
         "url": "https://orcid.org/0000-0001-5193-9200"
       }
     },
     {
       "@type": "Person",
       "name": "Nelson, A. R.",
       "givenName": "A. R.",
       "familyName": "Nelson",
       "identifier": {
         "@type": "PropertyValue",
         "propertyID": "ORCID",
         "value": "0000-0001-7117-7098",
         "url": "https://orcid.org/0000-0001-7117-7098"
       }
     },
     {
       "@type": "Person",
       "name": "Lund, W.R.",
       "givenName": "W.R.",
       "familyName": "Lund"
     }
   ]
 }

}