Figure 35. Curves showing the comparison of the coefficients
of the redundant lengths of the layers
l for the
geological sections of the anticlinoria and synclinoria
transverse the strike of the South Tien Shan fold system (see
Table 1 and 2).
(1) for the synclinoria (overall Hercynian and Alpine deformation);
(2) for the anticlinoria; (3) only for the Alpine synclinoria.
The names of the fold structural features: synclinoria: (A) Aravan,
(U) Uchkurgan, (OT) Okhna-Taldyk, (S) Surmetash, (DT) Daraut-Turkestan,
(KU) Kshtut-Urmeta, (FM) Fan-Margib, (ZK) Zidda-Karakul;
anticlinoria: (K) Kauzan, (KA) Kichikalai, (KH) Khodzhaachkan,
(ZT) Zeravshan-Turkestan, (ZR) Zeravshan Range, (G) Gissar.