Quburiga Fm
Type Locality and Naming
The type section is located in the West Hills of the Qubu region, Dingri County, Tibet. It was named by Yin Jixiang and Guo Shizeng in 1976.
Lithology and Thickness
Limestone and sandy shale. Composed of grey sandy shale and siltstone, intercalated with bioclastic limestone. It is divisible into three members: Lower member being composed largely of sandstone and siltstone, with a thickness of 40 m. Middle member representing interbeds of limestone and sandy shale, yielding abundant brachiopod fossils, with a thickness of 232 m. Upper member consisting chiefly of grey-black shale, with a thickness of 86 m. The total thickness is about 375.1 m.
Relationships and Distribution
Lower contact
Conformable contact with the underlying Qubu Fm
Upper contact
Disconformable contact with the overlying Baga Fm.
Regional extent
Distributed very extensively, and is found to occur in the West Hills of the Qubu Region, Dingri County, the Sure Mt., Gumu Trench, Xishan Mt. of the Selong Region of the Nyalam County, as well as in the vicinity of the Naxing County and in the area Gongda Region, Jilong County, and in the vicinity of Sarkujian Region of the Dingjie County.
GeoJSON
Fossils
It yields abundant marine animal fossils, including Brachiopods represented by the Taeniothaerus assemblage, the Calliomarginatia assemblage and the Chonetella assemblage; the Lytvolasma fauna of Corals, and Ammonoids represented by Uraloceras xizangensis.
Age
Depositional setting
Additional Information
GeoJSON estimate by Longgang Ye and Yuyin Li (Chengdu Univ. Tech. students)