Kamystin Fm
Type Locality and Naming
Along the Kamyshly River, Kuldyktau Mountains, Central Kyzylkum. Ya. B. Aysanov et al., 1968 (43, p. 66). In the monograph (165) - a synonym of the upper part of the Taushan Fm.
Synonym: Kamystinskaya Suite, Камыстинская св.
Lithology and Thickness
Sandstones, gravelites, shales, conglomerates, boulders, the composition of pebbles of which is mainly represented by terrigenous rocks of the underlying Taushan suite, limestones, and quartz. Thickness 500 m.
Relationships and Distribution
Lower contact
With erosion, angular, and azimuthal unconformity, it lies on the rocks of the Taushan Fm (44; 439). According to Yu.I. Loskikin (1986), it is a molasse composed of coarse clastic rocks - conglomerates, gravelites, boulders, lying above the Taushan Fm.
Upper contact
Schematic stratigraphic column indicates the upper contact as Tuzkoy Fm with erosion
Regional extent
Central Kyzylkum, in the form of isolated strips of NW extension in the central and eastern parts of the Kuldyktau Mountains.
GeoJSON
Fossils
In limestone pebbles, boulders, and blocks, crinoids are found - Kazakstanocrinus decemlobatus Yelt., K. cf. pennatus Sisova, Cupressocrinites ovatus Schew., Enthrochus cingulatus impares Quenst., Pentagonocyclicus katranensis Yelt. from the middle Devonian and Middle Carboniferous - Cyclocion cf. distinctus Moore et Left, Cyphostellechus elondus Moore et Left, found in Bashkirian and Lower Moscovian deposits; early Carboniferous foraminifera - Earlandia cf. elegans (Raus. et Reitl.), Endothyra ex gr. latispiralis Lip., E. sp., Spiroplectammina sp.; tabulates from the upper part of the Lower Devonian and Eifelian - Favosites cf. regularissimus minor Janet.
Age
Depositional setting
Additional Information