(a)
(b)
Figure 2:
(a) Expanded form of EPR spectrum of green dolomite at RT (
𝑣
=
9
.
3
9
1
2
8
G
H
z
). (b) Expanded form of EPR spectrum of white dolomite at RT (
𝑣
=
9
.
3
9
1
8
3
G
H
z
).
