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Sarmatian Craton
The
Sarmatian Craton
is a
geological
and
tectonics
term for the southern segment/region of the
East European Craton
also known as
Scythian Plateau
. The craton contains
Archaean
rocks 2.8 to 3.7 billion years old. During the
Carboniferous
Period the craton was
rifted
apart by the
Dneiper-Donets rift
. As a result,
geomorphologically
the cratonic area is split by the
Donbass
Fold Belt, also known as a part of the large
Pripyat-Dniepr-Donets aulacogen
, which transects Sarmatia, dividing it into the
Ukrainian Massif
or shield on the southwest and the
Voronezh Massif
to the northeast.
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