DOME, BASIN, PERICLINES
This is formed when early and late folds are both upright with
subvertical axial planes, the latter making a large angle with each other.
The axes of early and late folds are also at large angle to each other.
The domes and basins are not ideal but are elongated in the form of
elliptical domes and elliptical basins depending upon which folding is
more intense. The domes and basins will appear elongated in the direction
of early fold axial traces if the intensity of late folds is very mild and
that of early folds very strong. The reverse can also be true. It is not necessary that the two fold sets must cross at high angles to
each other. They may cross at moderate or low angles in which case the
folds tend to get arranged en echelon. The result is the formation of dome and basin outcrop pattern. On
denudation, they have the forms of eye shaped outcrops owing to the
intensity of one fold set being greater than the other. When antiforms of
early folds cross with antiforms of late folds, mutual culmination gives
rise to a domal structure. When synforms of the two generations cross each
other mutual depression gives rise to a basins. When early antiforms are
crossed by later synforms, the antiformal hinge of early fold is depressed
and when a synform of early generation is superimposed by an antiform of
later generation it causes culmination of the local synformal hinge giving
rise to structures called periclines. The photograph below shows the
periclines in the Zagros Mountains of Iran on regional scale, this picture
being a satellite photograph. |