Item talk:Q238005
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Apatite fission-track evidence for regional exhumation in the subtropical Eocene, block faulting, and localized fluid flow in east-central Alaska", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70168859", "url": "https://pubs.usgs.gov/publication/70168859" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70168859 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1139/cjes-2015-0138", "url": "https://doi.org/10.1139/cjes-2015-0138" } ], "journal": { "@type": "Periodical", "name": "Canadian Journal of Earth Sciences", "volumeNumber": "53", "issueNumber": "3" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Canadian Journal of Earth Sciences" } ], "datePublished": "2016", "dateModified": "2018-10-24", "abstract": "The origin and antiquity of the subdued topography of the Yukon\u2013Tanana Upland (YTU), the physiographic province between the Denali and Tintina faults, are unresolved questions in the geologic history of interior Alaska and adjacent Yukon. We present apatite fission-track (AFT) results for 33 samples from the 2300 km2 western Fortymile district in the YTU in Alaska and propose an exhumation model that is consistent with preservation of volcanic rocks in valleys that requires base level stability of several drainages since latest Cretaceous\u2013Paleocene time. AFT thermochronology indicates widespread cooling below \u223c110 \u00b0C at \u223c56\u201347 Ma (early Eocene) and \u223c44\u201336 Ma (middle Eocene). Samples with \u223c33\u201327, \u223c19, and \u223c10 Ma AFT ages, obtained near a major northeast-trending fault zone, apparently reflect hydrothermal fluid flow. Uplift and erosion following \u223c107 Ma magmatism exposed plutonic rocks to different extents in various crustal blocks by latest Cretaceous time. We interpret the Eocene AFT ages to suggest that higher elevations were eroded during the Paleogene subtropical climate of the subarctic, while base level remained essentially stable. Tertiary basins outboard of the YTU contain sediment that may account for the required >2 km of removed overburden that was not carried to the sea by the ancestral Yukon River system. We consider a climate driven explanation for the Eocene AFT ages to be most consistent with geologic constraints in concert with block faulting related to translation on the Denali and Tintina faults resulting from oblique subduction along the southern margin of Alaska.", "description": "21 p.", "publisher": { "@type": "Organization", "name": "National Research Council Canada" }, "author": [ { "@type": "Person", "name": "Dusel-Bacon, Cynthia cdusel@usgs.gov", "givenName": "Cynthia", "familyName": "Dusel-Bacon", "email": "cdusel@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-8481-739X", "url": "https://orcid.org/0000-0001-8481-739X" }, "affiliation": [ { "@type": "Organization", "name": "Geology, Minerals, Energy, and Geophysics Science Center", "url": "https://www.usgs.gov/centers/gmeg" } ] }, { "@type": "Person", "name": "O'Sullivan, Paul B.", "givenName": "Paul B.", "familyName": "O'Sullivan" }, { "@type": "Person", "name": "Bacon, Charles R. cbacon@usgs.gov", "givenName": "Charles R.", "familyName": "Bacon", "email": "cbacon@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-2165-5618", "url": "https://orcid.org/0000-0002-2165-5618" }, "affiliation": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ] }, { "@type": "Person", "name": "Day, Warren C. wday@usgs.gov", "givenName": "Warren C.", "familyName": "Day", "email": "wday@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-9278-2120", "url": "https://orcid.org/0000-0002-9278-2120" }, "affiliation": [ { "@type": "Organization", "name": "Geology, Minerals, Energy, and Geophysics Science Center", "url": "https://www.usgs.gov/centers/gmeg" }, { "@type": "Organization", "name": "Central Mineral and Environmental Resources Science Center", "url": "https://www.usgs.gov/centers/gggsc" }, { "@type": "Organization", "name": "Southwest Regional Director's Office", "url": "https://www.usgs.gov/regions/southwest" }, { "@type": "Organization", "name": "Mineral Resources Program", "url": "https://www.usgs.gov/programs/mineral-resources-program" } ] } ], "funder": [ { "@type": "Organization", "name": "Geology, Minerals, Energy, and Geophysics Science Center", "url": "https://www.usgs.gov/centers/gmeg" }, { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ], "spatialCoverage": [ { "@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/4074035" }, { "@type": "Place", "additionalType": "state", "name": "Alaska" }, { "@type": "Place", "additionalType": "unknown", "name": "Yukon\u2013Tanana Upland" }, { "@type": "Place", "geo": [ { "@type": "GeoShape", "additionalProperty": { "@type": "PropertyValue", "name": "GeoJSON", "value": { "type": "FeatureCollection", "features": [ { 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