Lolabulak Fm
Type Locality and Naming
In the eponymous southwestern part of the Kara-Tyube Mountains, where it is most widely developed. V.S. Korsakov in 1984 (1993) distinguished it from the Sarykul suite (460, p.63).
Synonym: Lolabulak Suite, Лолабулакская св.
Lithology and Thickness
Quartz-sericite slates, siliceous siltstone (aleurolites), sandstones with interlayers of conglomerates, limestones, plagioclase porphyrites, and their tuffs, rhyolites. Subvolcanic dikes and sills of liparite-porphyries are widely developed (thickness up to 70m). The formation is 1800 m thick.
Relationships and Distribution
Lower contact
Contacts are tectonic. Schematic stratigraphic column indicates the lower contact as Sarykul Fm
Upper contact
Contacts are tectonic. Schematic stratigraphic column indicates the upper contact as Atkamar Fm
Regional extent
Kara-Tyube Mountains.
GeoJSON
Fossils
Contains crinoids – Pentagonocyclicus elegans Yelt. and others; corals – Catenipora cf. tanaensis Sok. and others.
Age
Depositional setting
Additional Information