Pangduo Gr
Type Locality and Naming
The type section is located in the vicinity of the Pangduo Village, Linzhou County, Lhasa Region, Tibet. It was named by Li Pu in 1955.
Lithology and Thickness
Conglomerate. Composed of grey-green intermediate-basic volcanic breccia, quartz-sandstone, black pebble-bearing sandy slate. Thickness is 900 m.
Relationships and Distribution
Lower contact
Uncertain contact relationship with the underlying strata of Carboniferous Lading Gr.
Upper contact
Uncertain contact relationship with the overlying strata of Wululong Fm
Regional extent
Distributed in the vicinity of Lhasa, and the area from Mozhugongka to Naqu County, as well as the area of Buomi to Cayu Counties. In the Laigu area of the Buomi County the exposed Permian System used to be known as the Nacuo Gr (the 3rd Regional Geological Survey Party under the Sichuan Provincial Geological Bureau and the Nanjing Institute of Geology and Paleontology, 1982), among them that part which is corresponding to the Pangduo Gr is also known as the Yinga Fm and the Zhadongcuo Fm (Yin Jixiang, 1980), with a thickness of several hundreds of meters.
GeoJSON
Fossils
Its upper part yields abundant Brachiopods such as Bandoproductus, Chaiella, Leiorhynchoidea, Paeckmannella, Syringothyris, belonging to the Stepanoviella fauna,
Age
Depositional setting
It is interpreted as glacial marine-facies.
Additional Information
GeoJSON estimate by Longgang Ye and Yuyin Li (Chengdu Univ. Tech. students)