Dzhamsugum Fm
Type Locality and Naming
Along the Dzhamsugum uplift, Pre-Tashkent Chul. G.A.Belenky, 1966 (96, p.103). Stratotype in the southern part of the Dzhamsugum uplift, on the right bank of the Syrdarya River, 150 km from Tashkent.
Synonym: Dzhamsutum Suite, Джамсугумская св.
Lithology and Thickness
Greenish-light-gray, red clays, sandstones with layers of polymictic conglomerates and siltstone (aleurolites). Thickness 15-140m.
Relationships and Distribution
Lower contact
Lies with erosion on the Akdachin Fm and transgressively on the Paleozoic
Upper contact
It is overlain with erosion by the Syuksok Fm
Regional extent
Pre-Tashkent Chul, foothills of Chatkal, Karzhantau, and Kuramin ridges, in the Tashkent depression uncovered by drilling. Dzhamsugum Fm is an analog of the Urumbash Fm of S. Fergana.
GeoJSON
Fossils
Contains marine bivalve mollusks - Liostrea ex gr. delettrei Coq., Rhynchostreon chaperi Bayle, Gyrostrea longa (Bobk.); foraminifera - Gaudryinopsis asiaticus (N.Byk.), Haplophragmoides turonicus Zhuk., Brotzenella berthelini (Kell.), Hedbergella ex gr. holzli (Hagn.), Gavelinella aff. moniliformis (Reuss).
Age
Depositional setting
Additional Information