Vol. 311, Issue 9, 2011November 01, 2011 EDT
Zircon U-Pb Isotope, δ18O and Trace Element Response to 80 m.y. of High Temperature Metamorphism in the Lower Crust: Sluggish Diffusion and New Records of Archean Craton Formation
Zircon U-Pb Isotope, δ18O and Trace Element Response to 80 m.y. of High Temperature Metamorphism in the Lower Crust: Sluggish Diffusion and New Records of Archean Craton Formation
John R. Bowman, Desmond E. Moser, John W. Valley, Joseph L. Wooden, Noriko T. Kita, Frank K. Mazdab,
Bowman, J. R., Moser, D. E., Valley, J. W., Wooden, J. L., Kita, N. T., & Mazdab, F. K. (2011). Zircon U-Pb isotope, δ18O and trace element response to 80 m.y. of high temperature metamorphism in the lower crust: Sluggish diffusion and new records of Archean craton formation. American Journal of Science, 311(9), 719–772. https://doi.org/10.2475/09.2011.01