Figure 1. Photographs of fold dislocations in the territory of the
Turkestan Range, Southern Tien Shan.
A - an anticlinal fold in the sequence of
Lower Silurian cleavaged argillite and siltstone (Uab-Rawat
River valley, Shakhristan Pass area);
B - a synclinal fold in the sequence of cleavaged Lower Silurian shale
and siltstone (Uab-Rawat River valley;
C - a vertical anticlinal fold in the Lower Silurian cleavaged shale
and siltstone sequence (Argly R. Valley);
D - inclined anticline in the sequence of Lower Silurian shale and
siltstone (Shakhristan Pass area);
E - inclined anticline in the Lower Silurian sandstone and siltstone (Argly
R. Valley);
F - recumbent folds in the sequence of Lower Paleozoic shale and siltstone (Zaaminsu R. Valley);
G - a carinate syncline in Lower Silurian cleavaged shale and
siltstone (Argly R. Valley);
H - recumbent folds in the sequence
of Lower Paleozoic shale and siltstone (Zaaminsu R. Valley);
I - recumbent folds in the Lower Silurian
sandstones and siltstones (south of the Shakhristan Pass).
This document was generated by TeXWeb (Win32, v.1.3) on March 13, 2004.