Liubatang Fm
Type Locality and Naming
Central Yunnan. The Liubatang Fm was named by Deng Jiafan in 1961 and published by the Yunnan Bureau of Geology in 1966.The type locality is the area, south of Liubatang village, Jinning County, Yunnan Province. Coordinate: 24°38´12.6″N; 102°39´22.2″E. Middle formation in Bajie Gr.
[Figure: Type section of the Liubatang Fm]
Synonym: (留坝塘组)
Lithology and Thickness
It is subdivided into two parts. Lower part is composed of mainly black silty and muddy slate and carbonaceous slate, intercalated with siliceous slate and manganese-bearing slate. Its base is composed of purple-red ferruginous conglomerate with iron ore beds. Upward it is replaced by flesh-red thick-bedded dolomite (with stromatolites). Upper part consists of purple-red, yellow-green and pale blue silty slate, argillaceous slate intercalated with dark-grey chert. It is 255 m thick.
Relationships and Distribution
Lower contact
The base of the formation rests disconformably on the underlying Kunyang Gr (Luzhijiang Fm., but in localities it unconformably overlies the Heishan Fm or directly unconformably overlies on lower stratigraphic units like Meidang Fm. [Note: however, the succession of formations within the Kunyang Gr seems rather confused.] Elsewhere in east Yunnan, if the Liubatang Fm is considered as the middle formation within a Bajie Gr, then it is underlain by the lower one of Junshan Fm.
Upper contact
Its top is unconformably overlain by the Chengjiang Fm.
Regional extent
Central Yunnan. The Liubatang Fm occurs in a limited area, being seen in Junshao Village, Anning and in Jinning County.
GeoJSON
Fossils
Age
Depositional setting
Additional Information