Khodzhakul-Cret Fm
Type Locality and Naming
Named after the Khojakul village and lake, southern Pre-Aral region. S.S. Shultz (Jr.), 1967 (509, p.14). Stratotype at Hojakulsay (Khodzhakulsay), on the northwest slopes of Sultanuizdag Mountains.
Synonym: Khojakul Suite, Ходжакульская св.
Lithology and Thickness
Alluvial-deluvial cross-bedded sands, sandstones with interlayers of ferruginous conglomerates, gravelites, and clays, remains of turtle shells, scutes, and teeth; fragments of dinosaur bones; wood and bark of trees; shark teeth; vertebrae and scales of bony fish. The average thickness is 12-118 m.
Relationships and Distribution
Lower contact
It lies with erosion on the Kyzylkum Fm (Kyzylkalin Fm)
Upper contact
According to some, sometimes with erosion, it is overlain by the Beshtobin Fm
Regional extent
Sultanuizdag Range, Kokcha ranges, and adjacent regions of northwestern Kyzylkum.
GeoJSON
Fossils
Contains marine bivalve mollusks - Inoceramus crippsi Mant., Rhynchosreon chaperi (Bayle), Rh. orbicularum (Vinok.); shark teeth - Odontaspis macrorhiza Copr., Od. ex gr. sulcidens Copr., Scapanorhynchus ex gr. gracilis Ag., Sc. subulatus (Ag.), Ptychodus decurrens Ag.
Age
Depositional setting
Additional Information