Table 2

Microthermometric data.




ThV-L, [Crit]
Te
TmHH
TmI
TmC
ThTot




Sample
F.i. type
Origin
Range (Average ± 1σ)
N
Range (Average ± 1σ)
N
Range (Average ± 1σ)
N
Range (Average ± 1σ)
N
Range (Average ± 1σ)
N
Range (Average ± 1σ)
N

Dior-1
2b
P
-88
1
-32 to -51.7
8
n.o.

-4.2 to -12.8
10
5 to 9.2
12
277 to 326 (302 ± 14)
18
Dior-2
1
P
-100.1 to -122.9 (-119 ± 4)
42
-
-
-
-
-
-
-
-
-
-

2b
P
-86.3 to -113.6
13
-28.5 to -56.8 (-43 ± 7)
38
n.o.
-
-3.7 to -23.5 (-15 ± 5)
48
-0.7 to 10.1 (6.8 ± 2.7)
66
286 to 333 (312 ± 15)
17

2b
S
n.o.
-
n.o.
-
n.o.
-
-7
5
8 to 9
5
222 to 275
15
Dior-2
1
P
-83.5 to -101.9
14
-42 to -73.6 (-54 ± 7)
28
-4.6 to 20.8
16
-23.4 to -27.3 (-24.4 ± 0.7)
25
-3.2 to -7.1 (-5.5 ± 1)
19
288 to 385 (344 ± 15)
74
Gran-1b
2a
P
n.d.
-
n.d.
-
n.d.
-
n.d.
-
n.d.
-
215, 251
2

2a
S
n.o.
-
-45
1
3.4
1
-24
1
3.3
1
n.d.


2b?
P
-88.7 to -115.6
4
-
-
-
-
-
-
-
-
-
-
Slate-1a
1
P
-84.5 to -101.5 [-88, -88.7]
11 [2]
-48 to -76 (-55 ± 6)
23
-6.5 to 6.7
8
-22.8 to -25.6 (-24.4 ± 0.6)
25
-1.8 to -6.4 (-4.9 ± 1.2)
27
300, 322.5
2

2a
P
-101.1 [-85.1, -89, -103]
1 [3]
-39 to -52.8
10
-14.3, -4.1
2
-5.5 to -24.2
13
0.2 to 11.8
13
-
-

2b
P
n.o.
-
-45
1
n.o.
-
-9.3
1
9.2
1
252
1

2b
S
n.o.
-
-38 to -50.3
3
n.o.
-
-23.5, -25
2
n.o.
-
290 to 344 (319 ± 14)
26

2a or 2b
P
n.o.
-
-52
1
n.o.
-
-24
1
n.o.
-
230, 237, 261, 269
4

2a or 2b
S
-99.4 to -120.3
6
-
-
-
-
-
-
-
-
-
-
Slate-2
1
P
n.o.
-
-36, -63
2
n.o.
-
-3 to -22.8
8
-0.15 to 13.2
8
n.d.
-

2b?
P
-90, -90
2
-
-
-
-
-
-
-
-
-
-
Ves-1
1
P
n.o.
-
-30.6 to -42
10
n.o.
-
-4.5 to -5.3
12
4.8 to 10.8
5
n.d.
-

2c
P
n.o.
-
-37
1
n.o.
-
-4.2, -4.5, -5.7
3
n.o.
-
180 to 203
12
Ves-2
2c
P
-88
1
-32 to -51.7
8
n.o.
-
-4.2 to -12.8
10
5 to 9.2
12
277 to 326 (302 ± 14)
18

N: number of measurements, P: primary, S: secondary, T: temperature, h: homogenization, V-L: vapour to liquid, Crit: critical, e: first ice melting, m: melting, HH: hydrohalite, C: clathrate, Tot: total, n.o.: not observed, n.d.: not determined.

Normand and Williams-Jones Geochemical Transactions 2007 8:11   doi:10.1186/1467-4866-8-11