William Minarik

Coumans, J.P., Stix, J., Clague, D.A., Minarik, W.G., Layne, G.D., 2016. Melt-rock interaction near the Moho: Evidence from crystal cargo in lavas from near-ridge seamounts. Geochimica et Cosmochimica Acta 191, 139-164.

Martin, R.F., Alarie, E., Minarik, W.G., Waczek, Z., McCammon, C.A., 2016. Titanium-rich magnesio-hastingsite macrocrysts in a camptonite dike, Lafarge quarry, Montreal Island, Quebec: Early crystallization in a pseudo-unary system. Canadian Mineralogist 54 (1), 65-78.

Coumans, J.P., Stix, J., Clague, D.A., Minarik, W.G., 2015. The magmatic architecture of taney seamount-A, NE Pacific Ocean. Journal of Petrology 56 (6), 1037-1067. 

Kunzmann, M., Halverson, G.P., Scott, C., Minarik, W.G., Wing, B.A., 2015. Geochemistry of Neoproterozoic black shales from Svalbard: Implications for oceanic redox conditions spanning Cryogenian glaciations. Chemical Geology 417, 383-393.

Maneta, V., Baker, D.R., Minarik, W., 2015. Evidence for lithium-aluminosilicate supersaturation of pegmatite-forming melts. Contributions to Mineralogy and Petrology 170 (1), art. no. 416.

Sharman, E., Taylor, B., Minarik, W.,  Dubé, B. & Wing, B., 2015. Sulfur isotope and trace element data from ore sulfides in the Noranda district (Abitibi, Canada): implications for volcanogenic massive sulfide deposit genesis. Mineralium Deposita 50 (5), 591-606.

Cox, G.M., Halverson, G.P., Minarik, W.G., Le Heron, D.P., Macdonald, F.A., Bellefroid, E.J., Strauss, J.V. 2013, Neoproterozoic iron formation: An evaluation of its temporal, environmental and tectonic significance, Chemical Geology, vol. 362, pp. 232-249. 

Wilcock, J., Goff, F., Minarik, W.G., Stix, J. 2013, Magmatic recharge during the formation and resurgence of thevalles caldera, new mexico, usa: Evidence from quartz compositional zoning and geothermometry, Journal of Petrology, vol. 54, no. 4, pp. 635-664. 

Corgne, A., Armstrong, L.S., Keshav, S., Fei, Y., McDonough, W.F., Minarik, W.G., Moreno, K. 2012.  Trace element partitioning between majoritic garnet and silicate melt at 10-17GPa: Implications for deep mantle processes, Lithos, vol. 148, pp. 128-141. 

Campbell, M.E., Hanson, J.B., Minarik, W.G., Stix, J., 2009. Thermal history of the bandelier magmatic system: Evidence for magmatic injection and recharge at 1.61 Ma as revealed by cathodoluminescence and titanium geothermometry, Journal of Geology, 117 (5), 469-485.

Francis, D., Minarik, W., 2008. Aluminum-dependent trace element partitioning in clinopyroxene, Contributions to Mineralogy and Petrology, 156(4), 439-451.

Clarke, S.J., Hollmann, C.A., Zhang, Z., Suffern, D., Bradforth, S.E., Dimitrijevic, N.M., Minarik, W.G., Nadeau, J.L., 2006. Photophysics of dopamine-modified quantum dots and effects on biological systems, Nature Materials, 5(5), 409-417.

Wheeler, K.T., Walker, D., Fei, Y., Minarik, W.G., McDonough, W.F., 2006. Experimental partitioning of uranium between liquid iron sulfide and liquid silicate: Implications for radioactivity in the Earth's core, Geochimica et Cosmochimica Acta, 70(6), 1537-1547.

van Westrenen, W., Li, J., Fei, Y., Frank, M.R., Hellwig, H., Komabayashi, T., Mibe, K., Minarik, W.G., Van Orman, J.A., Watson, H.C., Funakoshi, K.-I., Schmidt, M.W., 2005. Thermoelastic properties of (Mg0.64Fe0.36)O ferropericlase based on in situ X-ray diffraction to 26.7 GPa and 2173 K, Physics of the Earth and Planetary Interiors, 151(1-2), 163-176.

Fei, Y., Li, J., Hirose, K., Minarik, W., Van Orman, J., Sanloup, C., van Westrenen, W., Komabayashi, T., Funakoshi, K.-I., 2004. A critical evaluation of pressure scale at high temperatures by in situ X-ray diffraction measurements, Physics of the Earth and Planetary Interiors, 143(1-2), 515-526.  

Fei, Y., Van Orman, J., Li, J., van Westrenen, W., Sanloup, C., Minarik, W., Hirose, K., Komabayashi, T., Walter, M., Funakoshi, K., 2004. Experimentally determined postspinel transformation boundary in Mg2SiO4 using MgO as an internal pressure standard and its geophysical implications, Journal of Geophysical Research B: Solid Earth, 109(2), B02305 1-8.