Related
Publication(s):
Davis, F. A., Cottrell, E., Birner, S. K., Warren, J. M., and Lopez, O. G., (2017), “Revisiting the electron microprobe method of spinel-olivine-orthopyroxene oxybarometry applied to spinel peridotites.” American Mineralogist, 102(2): 421–435;
Birner, S. K., Warren, J. M., Cottrell, E., Davis, F. A., Kelley, K. A., and Falloon, T. J., (2017), “Forearc peridotites from Tonga record heterogeneous oxidation of the mantle following subduction initiation.” Journal of Petrology, 58(9): 1755–1780;
Birner, S. K., Warren, J. M., Cottrell, E., and Davis, F. A., (2016), “Hydrothermal alteration of seafloor peridotites does not influence oxygen fugacity recorded by spinel oxybarometry.” Geology, 44(7): 535–538;
Birner, S. K., Cottrell, E., Warren, J. M., Kelley, K. A., and Davis, F. A., (2018), “Peridotites and basalts reveal broad congruence between two independent records of mantle fO2 despite local redox heterogeneity.” Earth and Planetary Science Letters, 494: 172–189;
Davis, F. A., and Cottrell, E., (2018), “Experimental investigation of basalt and peridotite oxybarometers: Implications for spinel thermodynamic models and Fe3+ compatibility during generation of upper mantle melts.” American Mineralogist, 103(7): 1056–1067;
Davis, F. A., and Cottrell, E., (2021), “Partitioning of Fe2O3 in peridotite partial melting experiments over a range of oxygen fugacities elucidates ferric iron systematics in mid-ocean ridge basalts and ferric iron content of the upper mantle.” Contributions to Mineralogy and Petrology, 176(9): 67;
User Contributed Keyword(s):
EPMA Methods, mantle, peridotite, oxygen fugacity, mid-ocean ridges, spinel