Item talk:Q50293

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usgs_staff_profile:

 meta:
   url: https://www.usgs.gov/staff-profiles/niki-wintzer
   timestamp: '2024-01-30T18:58:56.663002'
   status_code: 200
 profile:
   name: Niki Wintzer, PhD
   name_qualifier: null
   titles:
   - Research Geologist
   organizations:
   - !!python/tuple
     - Geology, Minerals, Energy, and Geophysics Science Center
     - https://www.usgs.gov/centers/gmeg
   email: nwintzer@usgs.gov
   orcid: 0000-0003-3085-435X
   intro_statements:
   - Niki is a Research Geologist in the Geology, Minerals, Energy, and Geophysics
     Science Center. In 2007, she joined the USGS in Menlo Park, CA but now works
     in Spokane, WA. She earned a B.S. in Earth Sciences from California Polytechnic
     State University in 2004, an M.S. in Geology from San Jose State University
     in 2009, and her Ph.D. in Geology from Washington State University in 2019.
   expertise_terms:
   - Ore Deposits
   - Geochronology & Geochemistry
   - Deformation (folding for example)
   - Sedimentary Rocks and Basins
   - Tectonic Processes
   - Structural Geology
   - Sedimentary Geology
   professional_experience:
   - 2009-present, Geologist, U.S. Geological Survey, Spokane, WA.
   - 2007-2009, Geologist, U.S. Geological Survey, Menlo Park, CA.
   education:
   - Ph.D. Geology, Washington State University, 2019
   - M.S. Geology, San Jose State University, 2009
   - B.S. Earth Sciences, California Polytechnic State University, 2004
   affiliations:
   - Geological Society of America (GSA) member
   - Society of Economic Geologists (SEG) member
   honors: []
   abstracts: []
   personal_statement: With specialized skills in geochronology, geochemistry, and
     structural geology, Niki investigates nationally important ore deposits. The
     Yellow Pine/Stibnite gold-antimony-tungsten mining area in central Idaho is
     her current research focus, and it holds the largest resource of the nationally
     critical commodity antimony. She is constraining the age of tungsten and antimony
     mineralization, unique geochemical signatures in the ore host rocks, and the
     ore-controlling structural setting that all provide insight into why mineralization
     formed when and where it did.