Shurasan Fm
Type Locality and Naming
Along the Shurasan anticline, foothills of the Gissar Range. G. Yu. Alferov et al., 1969.
Synonym: Shurasan Suite,
Lithology and Thickness
Unevenly alternating alluvial-proluvial brown-colored conglomerates, gravelites, sandstones, siltstone (aleurolites). Up to 1400 m.
Relationships and Distribution
Lower contact
With erosion lies on the Sulusay Fm and Paleogene
Upper contact
With erosion overlain by the Ammagan Fm.
Regional extent
Northern foothills of the Gissar Range, interfluve of the Tanhyzdarya and Kyzyl-Darya, Kashkadarya depression. Correlated with the Uchkolsay Fm in the southwestern Gissar. Correlated with the Kassantau Fm, Uchkolsay Fm, and Khodzhalychin Fm (144)
GeoJSON
Fossils
Contains ostracods - Ilyocypris ex gr. manasensis Mand., I. koktalensis Bodina., I. sp., Eucypris grandis Bodina., E. sp., Limnocythere depressa Schn., L. aff. botaschica Gr. in litt., L. ex gr. misera Mand., Candona merita Bodina, Candoniella albicans Br., Cyprinotus ex gr. arasensis Bodina., Mediocypris sp.
Age
Depositional setting
Additional Information