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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.