Progress in Earth and Planetary Science

Table 5 Fluorine and Chlorine partition coefficients from Dalou et al. ( [2012] ) and this study

From: Contrasting partition behavior of F and Cl during hydrous mantle melting: implications for Cl/F signature in arc magmas

Run	D _F	D _Cl
	Olivine
CD2H3	0.002(0.1)	0.003(4)
	Orthopyroxene
CD1 H0	0.123(4)	0.002(1)
CD2H3	0.056(0.3)	0.020(0.6)
CD2H5	0.042(4)	0.037(2)
CD2H6	0.021(31)	0.069(10)
CD1-2.5GPa	0.016(1)	0.002(0.2)
CD2-2.5GPa	0.046(1)	0.006(0.5)
	Clinopyroxene
CD1 H0	0.153(4)	0.009(0.5)
CD2H3	0.114(2)	0.011(1)
CD2H5	0.083(4)	0.015(0.8)
	Garnet
CD1-2.5GPa	0.012(0.4)	0.003(0.1)
CD2-2.5GPa	0.166(2)	0.087(4)
	Amphibole
CD2H4	0.360(66)	0.119(44)
CD2H6	0.635(87)	0.378(81)

Numbers in parentheses represent one standard deviation in terms of least units cited.
CD1 data presented to compare anhydrous and hydrous data.

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