Department of Geology
Dr. John R. Farver
Education & Experience:
Ph.D., Geological Sciences, Brown University (1988)
Specialty Areas of Interest:
Current BGSU Courses:
Earth Environments – Ugrad
Recent and Current Research or Grants:
Farver and Miner, (Co-PI’s) "Otolith Microchemistry as a Natural Tag for Mixed Stock Analysis of Hatchery Reared Steelhead", NOAA Ohio SeaGrant Program, $180k awarded.
Farver and Miner (Co-PI's) “Quantifying the Role of Mayflies (Hexagenia) in the Trophic Transfer of Persistent Bioacumulative Toxic Metals in the Western Basin of Lake Erie", Lake Erie Protection Fund, award $10k, 12/06.
Farver and Miner, (Co-PI’s) “Employing Trace Element Contents of Otoliths for Fish Stock Discrimination and Habitat Use", NOAA, Ohio Sea Grant Program, award $173k, 4/2005.
Recent Peer Reviewed Publications and Submissions:
Gorsevski P. V., Onasch C. M., Farver J. R., and Ye X. (accepted). Detecting grain boundaries in deformed rocks using a cellular automata approach. Computers & Geosciences.
O’Kane, A., Onasch, C. M., and Farver, J. R. (2007) The role of fluids in low temperature, fault-related deformation of quartz arenite. J. Structural Geol., 29, 819-836.
Farver J. R. and Brabander, D. J. (2001) Magma ascent rates from mineral reaction rims and extension to teaching about volcanic hazards. J. Geoscience Education, 49, 140-145.
Farver J. R. and Yund R. A. (2000) Silicon diffusion in a natural quartz aggregate: constraints on solution-transfer diffusion creep. Tectonophysics, 325, 191-203.
Farver J. R. and Yund R. A. (2000) Silicon diffusion in forsterite aggregates: implications for diffusion creep. Geophysical Research Letters 27, 2337-2340.
Farver J. R. and Yund R. A. (1999) Oxygen bulk diffusion measurements and TEM characterization of a natural ultramylonite: implications for fluid transport in mica-bearing rocks. J. Metamorphic Geol. 17, 669-683.
Farver J. R. and Yund R. A. (1998) Oxygen grain boundary diffusion in natural and hot-pressed calcite aggregates. Earth Planet. Sci. Lett. 161, 189-200.