Upper Cambrian Fm
Type Locality and Naming
Synonym: Upper Division
Reference section:
Lithology and Thickness
Clay slates, claystones, limestones. It is represented by alternations of dark gray clay slates, claystones, limestones, and sandstones, which contain rare lenses of conglomerates. The thickness is 200 m. The number of slates increases up the section. At the bottom, coarse-grained sandstones and conglomerates usually predominate, containing (Yaskovich, 1968) in the pebbles remains of trilobites of the Mayan stage.
Relationships and Distribution
Lower contact
On the rocks of the Mayan stage, the upper Cambrian lies with erosion, but without angular discordance.
Upper contact
It is overlain by terrigenous rocks of the Lower Ordovician in conformity.
Regional extent
It is widespread in the same locations as the middle division i.e., in Central Tajikistan (Zeravshan-Gissar and South Gissar districts) and in the Northern Pamir.
GeoJSON
Fossils
In the interlayers of limestones and carbonate cement of conglomerates, there are trilobites characteristic of the upper Cambrian: Homagnostus obesus Belt., H. asiaticum Hajr., Lisania sp., Onchonotellus oburdonicus Hajr., Prochuangia minuscula Hajr., Proceratopyge schaganica Hajr,, and others (Geol. USSR, vol. 23, 1972).
Age
Depositional setting
Additional Information