Koksuy Fm
Type Locality and Naming
Along the Koksu River, Chatkal River basin, Chatkal Ridge. O.I. Sergun'kova, 1959 (382, p. 63). Stratotype on the Kulosey River, left tributary of the Koksu River, near the village of Burchmulla.
Synonym: Koksu Suite, Коксуйская св.
Lithology and Thickness
The suite is divided into two parts. Lower - gray layered, nodular, nodular, aphanitic limestones with characteristic small "eyes" of transparent calcite. Thickness up to 200m. Upper - thick- to medium-bedded dark gray to black limestones, predominantly organogenic-detrital. Thickness 40-80m.
Relationships and Distribution
Lower contact
Along V.V. Mikhailov (460), it lies conformably on the Temirbastau Fm, and when this suite is completely absent from the section, it lies conformably on Devonian deposits
Upper contact
It is conformably overlain by the Taldybulak Fm or its analogue - the Kulosey Fm
Regional extent
Ugam, Pskem, and Koksu Ridges. Laterally, on the left bank of the Chatkal River (Chatkal River basin), it is replaced by massive limestones of the Akbulak Fm and reefoid masses of the "Akbulak" type.
GeoJSON
Fossils
Contains numerous crinoid remains; brachiopods - Palaeochoristites čatkalicus Dik., foraminifera - Septabrunsiina donica Lip., Endothyra parakosvensis Lip.; conodonts - Siphonodella crenulata Coop., S. isosticha (Coop.), S. obsoleta Hass.
Age
Depositional setting
Additional Information