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<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>Warren C. Day</dc:contributor>
  <dc:contributor>John N. Alienikoff</dc:contributor>
  <dc:contributor>Richard W. Saltus</dc:contributor>
  <dc:contributor>Larry P. Gough</dc:contributor>
  <dc:contributor>Warren C. Day</dc:contributor>
  <dc:creator>J. Michael O’Neill</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>The Black Mountain tectonic zone in the YukonTanana terrane of east-central Alaska is a belt of diverse 
northeast-trending geologic features that can been traced 
across Black Mountain in the southeast corner of the Big Delta 
1&amp;deg;×3&amp;deg; degree quadrangle. Geologic mapping in the larger 
scale B1 quadrangle of the Big Delta quadrangle, in which 
Black Mountain is the principal physiographic feature, has 
revealed a continuous zone of normal and left-lateral strikeslip high-angle faults and shear zones, some of which have 
late Tertiary to Quaternary displacement histories. The tectonic 
zone includes complexly intruded wall rocks and intermingled 
apophyses of the contiguous mid-Cretaceous Goodpaster and 
Mount Harper granodioritic plutons, mafic to intermediate 
composite dike swarms, precious metal mineralization, early 
Tertiary volcanic activity and Quaternary fault scarps. These 
structures define a zone as much as 6 to 13 kilometers (km) 
wide and more than 40 km long that can be traced diagonally across the B1 quadrangle into the adjacent Eagle 1&amp;deg;×3&amp;deg; 
quadrangle to the east. Recurrent activity along the tectonic 
zone, from at least mid-Cretaceous to Quaternary, suggests 
the presence of a buried, fundamental tectonic feature beneath 
the zone that has influenced the tectonic development of 
this part of the Yukon-Tanana terrane. The tectonic zone, 
centered on Black Mountain, lies directly above a profound 
northeast-trending aeromagnetic anomaly between the Denali 
and Tintina fault systems. The anomaly separates moderate 
to strongly magnetic terrane on the northwest from a huge, 
weakly magnetic terrane on the southeast. The tectonic zone is 
parallel to the similarly oriented left-lateral, strike-slip Shaw 
Creek fault zone 85 km to the west.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/sir20075289D</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>The Black Mountain tectonic zone--a reactivated northeast-trending crustal shear zone in the Yukon-Tanana Upland of east-central Alaska: Chapter D in &lt;i&gt;Recent U.S. Geological Survey studies in the Tintina Gold Province, Alaska, United States, and Yukon, Canada--results of a 5-year project&lt;/i&gt;</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>