RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES6002, doi:10.2205/2005ES000187, 2005

Figure 9. The tectonic structure of the Zidda Basin (its central and eastern parts): (1) the dolomite,
limestone, and greenschist of the Yagnob tectonic zone (Ordovician-Silurian); (2) the shale and sandstone
(flysch) of the Maikhura Formation (Middle-Late Carboniferous); (3-10) the rocks of the Zidda Formation
(Moscow Stage of the Middle Carboniferous to the Late Carboniferous, possibly, the Early Permian, as
suggested in [Leonov, 1995]: (3) shale and sandstone with landslide breccia interbeds,
(4) shale, siltstone, and sandstone, (5) sandstone and conglomerates, (6) sandy-clayey rock sequences
of chaotic structure (gravitational mixtite); (7) carbonate breccia; (8) interbeds of pelitomorphic ooze
and algal limestone; (9) limestone slabs in sandstone and shale sequences; (10) marble; (11) Devomian and
Lower-Middle Carboniferous limestone (synsedimentation tectonic nappes); (12) transgressively overlapping
Mesozoic rocks and markers; (13) granodiorite and diorite; (14) tectonic crush zone; (15) overthrust and
other faults.

Citation: Leonov, M. G. (2005), The Post-Oceanic Geodynamics of the South Tien Shan Region, Russ. J. Earth Sci., 7, ES6002, doi:10.2205/2005ES000187.
Copyright 2005 by the Russian Journal of Earth Sciences
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