Tonashin Fm
Type Locality and Naming
Along the Tona Mountain, Mangyshlak Peninsula. T.A. Ishina, 1961 (476, p.219). Tonashin Fm is exposed by wells in South Mangyshlak, South Turkmenistan, and analogs on Ustyurt. Stratotype on Tona Mountain (446). In South Ustyurt, it was distinguished (383, table 4, sheet 2) as the Lower Tona subsuite (see Takhtakair Fm) and undivided Upper Tona subsuite and Karadiirmen Fm (see Berdak Fm).
Synonym: Tonashinskaya Suite, Тонганинская св.
Lithology and Thickness
Divided into two subsuites (91; 383, table 4, sheet 2).
Upper Tona subsuite - alternation of sandy and silty (aleurolitic) clayey rocks with coal seams. Thickness 40m.
Lower Tona subsuite - cross-bedded polymictic sandstones with lenses of conglomerates. Thickness up to 230m.
Relationships and Distribution
Lower contact
Upper Tona subsuite - Along the stratigraphy, it lies on the Lower Tona subsuite
Lower Tona subsuite - Lies with erosion on the Paleozoic or Kokalin Fm
Upper contact
Upper Tona subsuite – is transgressively overlain by the Karadiirmen Fm
Lower Tona subsuite – overlain with erosion by the Upper Tona subsuite.
Regional extent
Eastern part of the Mangyshlak Peninsula, in the Tona uplift area, Kelendy area near the Kugusem village
GeoJSON
Fossils
Upper Tona subsuite – Contains freshwater bivalve mollusks - Subcardinia sibirensis Mart., Pseudocardinia lacustris Kol. and others; large plant remains Coniopteris angustiloba Brick, Phlebopteris polypodioides Brongn. and others.
Lower Tona subsuite – Contains spore and pollen assemblages (see Takhtakair Fm).
Age
Depositional setting
Additional Information