Figure 31. Map of morphological folding types in the central
segment of the South Tien Shan region. (1) Mesozoic and Cenozoic
rocks; (2-5) zones of different morphologic folding types: (2) compressed,
isoclinal, and carinate folds (tightness scale
(t.s.)=0.8-1.0); (3) less compressed linear folds (t.s.)=0.6-0.75;
(4) arc-shaped and crestlike folds (t.s.)=0.25-0.55;
(5) box-like, trough-shaped folds and flexures (t.s.)=0.1-0.2;
(6) zones of overthrust structure; (7-9) intrusive rock massifs:
(7) ultrabasic rocks, (8) granitoids, (9) alkaline rocks;
(10) boundaries of large fold structures (anticlinoria and
synclinoria); (11) same, coinciding with regional thrust faults;
(12) boundaries between zones of different folding morphology;
(13) same, coinciding with thrust faults; (14) lines of
geological sections used; (15) greenschist (metamorphic)
rocks; (16) metamorphic rocks (crystalline schist, gneiss,
greenschist) of the Turkestan metamorphic zone.
Anticlinoria: (I) Kauzan, (II) Kichikalai,
(III) Khodzhaachkan, (IV) Zeravshan-Turkestan, (IVa) Turkestan
metamorphic zone, (V) Malguzar, (VI) Zeravshan Range,
(VII) Gissar.
Synclinoria: (VIII) Aravan, (IX) Uchkurgan, (X) Okhna-Taldyk,
(XI) Zaama, (XII) Surmetash, (XIII) Daraut-Turkestan (Kurganak),
(XIV) Kshtut-Urmeta, (XV) Fan-Margib, (XVI) Ziddy-Karakul, (XVII) South
Gissar structure-formation zone.