Harzburgite melting with and without H2O: Experimental data and predictive modeling

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The effect of H2O on the olivine liquidus of basaltic melts: experiments and thermodynamic models (2008, methodology): “Most of our experiments have been performed between 0 and 200 MPa, whereas data by Gaetani and Grove (1998) and Parman and Grove (2004) are in the 1.2–2.0 GPa pressure range.”
Intercalibration of FTIR and SIMS for hydrogen measurements in glasses and nominally anhydrous minerals (2007, methodology): “For example, the olivine and orthopyroxene standards were characterized by FTIR using unpolarized measurements and the calibration of Paterson (1982).”
The Role of Water in Generating the Calc-alkaline Trend: New Volatile Data for Aleutian Magmas and a New Tholeiitic Index (2010, background): “…mantle melting at low pressures (Kushiro, 1972; Albare' de, 1992; Rogers et al., 1995; Lee et al., 2009), equilibration of melt with harzburgite (Parman & Grove, 2004; Grove et al., 2005), high-pressure fractionation in the presence of garnet (Macpherson et al., 2006), and low-degree melting of…”