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Table 3 Comparison of volatile elements’ composition of experimental run products between 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

Samples Phase H 2 O (wt.%) F (ppm) Cl (ppm)
Dalou et al. ( [2012] )     
CD1 H0 Glass [4] 0.17(0.3) 101(1) 8,515(57)
  Opx [3] 0.10(1) 14(0.3) 19(3)
  Cpx [3] 0.05(0.3) 16(0.3) 77(4)
CD1-2.5GPa Glass [5] 0.79(2) 6,406(122) 4,772(93)
  Grt [12] 0.47(1) 73(1) 13(0.3)
  Opx [4] 0.49(1) 121(4) 13(1)
  Cpx [4] 0.39(1) 319(4) 10(0.4)
This study     
CD2H3 Glass [3] 2.59(1) 18,241(64) 3,491(13)
  Opx [5] 0.20(1) 1,203(42) 83(2)
  Cpx [3] 0.21(0.2) 2,319(22) 44(3)
  Ol [6] 0.10(0.2) 33(1) 9(1)
CD2H4 Glass [3] 4.33(29) 146,867(17,657) 405(68)
  Amph [4] 1.27(0.2) 62,264(2,214) 57(8)
CD2H5 Glass [3] 4.89(3) 14,765(385) 2,491(10)
  Opx [3] 0.49(1) 668(35) 99(3)
  Cpx [4] 0.55(1) 1,185(23) 35(2)
CD2H6 Glass [2] 5.88(29) 119,267(10,293) 640(72)
  Opx [3] 1.12(17) 2,001(24) 35(3)
  Amp [3] 4.43(1) 62,959(5,033) 201(29)
CD2-2.5GPa Glass [2] 1.58(1) 7,647(42) 3,379(13)
  Grt [5] 0.52(2) 986(12) 229(14)
  Opx [3] 0.45(1) 352(5) 22(2)
  1. Numbers in brackets indicate number of individual ion probe analyses included in average.
  2. Numbers in parentheses represent one standard deviation in terms of least units cited.
  3. b.d.l. below detection limits.