Barovich, K. M. (1991). Neodymium isotopic evidence for early Proterozoic units in the Watersmeet gneiss dome, northern Michigan. Temperature-pressure estimates of dynamically recrystallized rocks in the early Proterozoic Mountain shear zone, northeastern Wisconsin. U.S. Department of the Interior, U.S. Geological Survey.
Chicago Style (17th ed.) CitationBarovich, Karin M. Neodymium Isotopic Evidence for Early Proterozoic Units in the Watersmeet Gneiss Dome, Northern Michigan. Temperature-pressure Estimates of Dynamically Recrystallized Rocks in the Early Proterozoic Mountain Shear Zone, Northeastern Wisconsin. [Reston, Va.]: U.S. Department of the Interior, U.S. Geological Survey, 1991.
MLA (9th ed.) CitationBarovich, Karin M. Neodymium Isotopic Evidence for Early Proterozoic Units in the Watersmeet Gneiss Dome, Northern Michigan. Temperature-pressure Estimates of Dynamically Recrystallized Rocks in the Early Proterozoic Mountain Shear Zone, Northeastern Wisconsin. U.S. Department of the Interior, U.S. Geological Survey, 1991.