<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>J.M. Murphy</dc:contributor>
  <dc:creator>Cynthia Dusel-Bacon</dc:creator>
  <dc:date>2001</dc:date>
  <dc:description>&lt;div class="box-pad border-lightgray margin-bottom"&gt;&lt;div&gt;&lt;div class="abstractSection"&gt;&lt;div class="abstractSection abstractInFull"&gt;&lt;p class="first last"&gt;We present an apatite fission-track (AFT) study of five plutonic rocks and seven metamorphic rocks across 310 km of the YukonTanana Upland in east-central Alaska. Samples yielding ~40 Ma AFT ages and mean confined track lengths &amp;gt; 14 µm with low standard deviations cooled rapidly from &amp;gt;120°C to &amp;lt;50°C during a 35 Ma period, beginning at about 40 Ma. Data from samples yielding AFT ages &amp;gt;40 Ma suggest partial annealing and, therefore, lower maximum temperatures (~90105°C). A few samples with single-grain ages of ~20 Ma apparently remained above ~50°C after initial cooling. Although the present geothermal gradient in the western YukonTanana Upland is ~32°C/km, it could have been as high as 45°C/km during a widespread Eocene intraplate magmatic episode. Prior to rapid exhumation, samples with ~40 Ma AFT ages were &amp;gt;3.82.7 km deep and samples with &amp;gt;50 Ma AFT ages were &amp;gt;3.32.0 km deep. We calculate a 440320 m/Ma minimum rate for exhumation of all samples during rapid cooling. Our AFT data, and data from rocks north of Fairbanks and from the Eielson deep test hole, indicate up to 3 km of post-40 Ma vertical displacement along known and inferred northeast-trending high-angle faults. The predominance of 4050 Ma AFT ages throughout the YukonTanana Upland indicates that, prior to the post-40 Ma relative uplift along some northeast-trending faults, rapid regional cooling and exhumation closely followed the Eocene extensional magmatism. We propose that Eocene magmatism and exhumation were somehow related to plate movements that produced regional-scale oroclinal rotation, northward translation of outboard terranes, major dextral strike-slip faulting, and subduction of an oceanic spreading ridge along the southern margin of Alaska.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1139/cjes-38-8-1191</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Canadian Science Publishing</dc:publisher>
  <dc:title>Apatite fission-track evidence of widespread Eocene heating and exhumation in the Yukon-Tanana Upland, interior Alaska</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>