Mazzanchut Fm
Type Locality and Naming
It was distinguished in 1949 by B. P. Barhatov, who considered it conditionally Lower Paleozoic.
Synonym: Mazzanchut suite, Маэанчутская свита
Reference section:
Lithology and Thickness
The primary rocks of this suite were likely mainly volcano-clastic; later, they underwent greenstone metamorphosis. The suite is composed of green albite-biotite-actinolite schists, including layers and lenses of white marbles, marbled limestones, mica schists, and amphibolites. The incomplete thickness of the suite is 500 m.
Relationships and Distribution
Lower contact
Upper contact
Carboniferous (?) - Triassic and Jurassic rocks
Regional extent
It is widespread in the Rushan range.
GeoJSON
Fossils
No organic remains have been found in it.
Age
Depositional setting
Additional Information