|
Temperature, °C
|
pH
|
Na, mg/L
|
K, mg/L
|
Mg, mg/L
|
Ca, mg/L
|
Cl, mg/L
|
HCO3, mg/L
|
SO4, mg/L
|
Li, mg/L
|
Br, mg/L
|
Br/Cl, molar ratio, × 10−3
|
δD, ‰
|
δ18O, ‰
|
References
|
---|
KDE
|
12
|
7.8
|
14,000
|
180
|
66
|
650
|
24,000
|
66
|
0
|
83
|
41
|
0.75
|
− 52
|
− 2
|
Present study
|
Arima end-member
|
>138
|
–
|
25,900
|
5250
|
0.09
|
5020
|
54,000
|
–
|
–
|
78
|
115
|
0.92
|
− 32
|
10
|
Masuda et al. (1985)
|
–
|
–
|
21,000
|
3700
|
–
|
3100
|
42,000
|
–
|
–
|
55
|
84
|
2.0
|
− 33
|
6
|
Kusuda et al. (2014)
|
Fluid inclusions
|
–
|
–
|
–
|
600 ~ 3700
|
–
|
–
|
12,000 ~ 240,000
|
–
|
–
|
–
|
27 ~ 2000
|
1.0 ~ 3.7
|
–
|
–
|
Kendrick et al. (2011)
|
–
|
–
|
5400 ~ 53,000
|
1100 ~ 57,000
|
N.D. ~ 20,000
|
N.D. ~ 16
|
–
|
–
|
–
|
N.D. ~ 49
|
–
|
–
|
–
|
–
|
Fukuyama et al. (2017)
|
- KDE is extrapolated as described in the text. The composition of the Arima brine end-member is from Masuda et al. (1985) and Kusuda et al. (2014), and those of fluid inclusions are from Kendrick et al. (2011) and Fukuyama et al. (2017)