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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>Richard J. Goldfarb</dc:contributor>
  <dc:contributor>Philip L. Verplanck</dc:contributor>
  <dc:contributor>Thomas P. Trainor</dc:contributor>
  <dc:contributor>Richard F. Sanzolone</dc:contributor>
  <dc:contributor>Monique Adams</dc:contributor>
  <dc:contributor>Larry P. Gough</dc:contributor>
  <dc:contributor>Warren C. Day</dc:contributor>
  <dc:creator>Seth H. Mueller</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>Epigenetic mineral deposits in the Tintina Gold Province 
are generally characterized by high concentrations of arsenic 
and antimony in their mineral assemblage. A total of 347 samples (ground water, surface water, and stream sediment) were 
collected to investigate the distribution and mobility of arsenic 
and antimony in the environment near known mineral deposits. Samples were collected from east to west at Keno Hill and 
Brewery Creek, Yukon, Canada; and Cleary Hill, True North, 
Scrafford Mine, Fairbanks, Ryan Lode, Stampede Creek, 
Slate Creek, and Donlin Creek, all in Alaska. Surface- and 
ground-water samples are all slightly acidic to near-neutral 
in pH (5-8), have a wide range in specific conductance 
(surface water 17-2,980 microsiemens per centimeter and 
ground water 170-2,940 microsiemens per centimeter), and 
show elevated dissolved arsenic and antimony concentrations 
(arsenic in surface water is less than 1 to 380 micrograms per 
liter and in ground water is less than 1 micrograms per liter to 
1.5 milligrams per liter; antimony in surface water is less than 
2 to 660 micrograms per liter and in ground water is less than 
2 to 60 micrograms per liter). Stream sediments downstream 
from these deposits have high concentrations of arsenic and 
antimony (arsenic median is 1,670 parts per million, maximum is 10,000 parts per million; antimony median is 192 
parts per million, maximum is 7,200 parts per million). The 
mobility of arsenic and antimony is controlled by the local 
redox environment, with arsenic being less mobile in oxidized 
surface waters relative to antimony, and arsenic more mobile 
in reduced ground water. These factors suggest that both antimony and arsenic may be useful pathfinder elements in water 
and sediment for targeting similar style deposits elsewhere in 
the Tintina Gold Province.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/sir20075289G</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Surface-water, ground-water, and sediment geochemistry of epizonal and shear-hosted mineral deposits in the Tintina Gold Province--arsenic and antimony distribution and mobility: Chapter G 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>