GMEG - Mineral and Environmental Resources
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Niki E. Wintzer's Publications | |
Interests: |
Economic Geology: sediment-hosted copper deposits, porphyry copper deposits, and volcanogenic massive sulfide deposits |
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Structural Geology: ductile deformation of the mid to deep crust including refolded folds and kinematic microstructures, and the insights they provide into the paleo-strain field
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Sedimentology: carbonate nodules and their paleoenvironmental implications |
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Contact: |
509-368-3110 |
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Education |
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| 2004 – B.S. Earth Sciences, California Polytechnic State University | ||
| 2009 – M.S. Geology, San Jose State University | ||
Experience |
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I joined the USGS in 2007 when I began assisting Cynthia Dusel-Bacon with her extensive and fascinating research of east-central Alaskan geology and its associated mineral deposits. Subsequent assessment work with Dr. Steve Ludington exposed me to the world-class mineral deposits in the basin-and-range province of Northern Nye County, Nevada. Additionally, I was able to study the complicated structure of the Brooks Range on the north slope of Alaska as a field assistant to Dr. Thomas Moore during the summer of 2009. As of December 2009, the Spokane, Washington Minerals office has become my permanent home where I use my numerous geologic skills to assess mineral potential worldwide. My geologic career began in the summer of 2002 when I participated in a Research Experience for Undergraduates (REU) funded by the National Science Foundation (NSF) led by Dr. Julie Maxson. During this research experience, I did 5 weeks of field work in Dinosaur National Monument, subsequently performed independent academic and laboratory research, and presented that research at the national GSA meeting that fall. My undergraduate senior thesis came from this research and is titled “Paleoenvironmental Implications of Carbonate Nodules.” The Sauropod found in the Cedar Mountain Formation lived in an arid to semi-arid climate, which was an unexpected but interesting conclusion because most Sauropods are envisioned in lush tropical climates. While earning my M.S. in Geology, I analyzed the structure of the mid to deep crust exposed as part of the Skagit Gneiss Complex in the North Cascades, Washington under the tutelage of Dr. Robert Miller. Multiple deformational episodes, including three fold generations, were separated out, and episode age was constrained in conjunction with on-going geochronological studies of the Skagit Gneiss Complex. Domains of top-to-the-NW and top-to-the-SE shear were revealed and correlated with lower (300-400 ˚C) and higher (≥450 ˚C) deformation temperature domains, respectively. Two geologic maps and a 72-page thesis were the products of this research. |
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Current Activities |
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Return to Spokane office
| Mineral Resources | Eastern / Central / Western / Alaska / Minerals Information |
| Crustal Geophysics and Geochemistry / Spatial Data |