Fand Fm
Type Locality and Naming
Synonym: Fand suite, Фанекая свита
Reference section:
Lithology and Thickness
In the lower part is made up of lens-shaped interbedding of cross-bedded gravelites-breccias, coarse-grained quartz sandstones, fine-gravel conglomerates. In the upper part, the sorting of material improves, conglomerates are observed less frequently; among the gravel-sandy rocks, there are interlayers of claystones. The thickness of the suite is 60-115 m.
Relationships and Distribution
Lower contact
The considered deposits lie either sharply unconformably on the rocks of the Paleozoic, or with a slight erosion on the formations of the Ravat Fm previously attributed to the Upper Triassic deposits, and according to our and R.Z. Gengkina's data, included in the Lower Triassic section.
Upper contact
It is overlain by Cretaceous red beds with an unclear contact.
Regional extent
GeoJSON
Fossils
In the upper half of the suite, the author has collected and identified plant remains of Neocalamites sp., Phlebopteris braunii Goepp., Thaumatopteris hissarica Brick, Hissaropteris jagnobensis Kuz. et Sixt., Cladophlebis sp., Coniopteris hymenophylloides (Brongn.) Sew., Ginkgo ferganensis Brick, etc.
Age
Depositional setting
Additional Information