Geoscience Reference
In-Depth Information
40
y = 2.5711 + 0.0236
x
+ 2.726e-4
x
^
2 R - 0.93
30
20
10
0
20
y - 5.3585 + 0.0994
x
- 2.288e-4
x
^
2 R - 0.83
15
10
5
0
40
y - 0.0785 - 0.0203
x
+ 4.449e-4
x
^
2 R - 0.91
30
20
10
0
100
y - 5.1522 - 0.1207
x
+ 0.0015
x
^
2 R - 0.90
80
60
40
20
0
40
y - 0.9485 + 0.0256
x
+ 2.656e -4
x
^
2 R = 0.88
30
20
10
0
0
50
100
150
Age (ka)
200
250
Fig. 11.2
Examples of soil chronofunctions from the central and southern Transantarctic
Mountains (Bockheim
1990
)
