Figure 5
From: Large-ion lithophile elements delivered by saline fluids to the sub-arc mantle
Comparison of the present partition coefficients with previous works. (A, B, C) Partition coefficients as a function of NaCl + KCl in haplogranite-H2O. Comparison with previous works using in situ analysis (Bureau et al. 2007; Borchert et al. 2009, 2010a) is discussed in the text. Numbers represent experimental pressure in GPa. (D, E, F) Partition coefficients as a function of NaCl + KCl in haplogranite-H2O. Comparison with previous works using quench experiments (Keppler 1996; Bai and Koster van Groos 1999) is discussed in the text. Experimental pressure by Keppler (1996) and by Bai and Koster van Groos (1999) is 0.3 and 0.2 GPa, respectively. The pressures in the present study are shown in (A, B, C).