fig31.htm

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.


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