fig07.htm

Figure 7. Schematic structural map of the Baubashata Mountains: (1-4)  Lower and Middle Paleozoic rocks: (1) greenschist complex of metamorphic island-arc rocks, (2) unmetamorphozed island-arc volcanics, (3) serpentinized ultrabasic rocks, (4) condensed terrigenous silicic (paleo-oceanic-type) rocks; (5) shelf-type (autochthonous) limestones and dolomites; (6) Mesozoic and Cenozoic sediments; (7) Late Paleozoic molasse; (8) granitoids; (9) Middle Tien Shan structure-formation zones (Chatkal-Kurama Fold System); (10) North Tien Shan structure-formation zones; (11) nappes; (12) overthrusts; (13) strike-slip faults, (14) other faults; (15-16) large folds: (15) anticlines (and anticlinoria), and (16) synclines (and synclinoria). The names of the largest fold-type structural features: (1) Sarybel Megasyncline, (2) Ryazan megaanticline, (3) Kerey Megasyncline, (4) Isfandzhailoos Megasyncline, (5) Kainda Megaanticline, (6) Seresui megaanticline, (7) Mailisui Megasyncline. A-B is the line of the section shown in Figure 8.


This document was generated by TeXWeb (Win32, v.1.3) on March 13, 2004.