Geology Reference
In-Depth Information
Figure 2.24
(Cont.)
of “transitional” chlorine-magnesium and sulphate-sodium
varieties with secondary salinity factor 0.1
3.5%-equiv. The
lateral change in water type within the same interval from
the structures' crests to their flanks and plunges occurs by
zones, through areals of “transitional” chlorine-magnesium,
−
