Shiyingliang Fm
Type Locality and Naming
North-central Qinghai. The Shiyingliang Formation was named by Wang Yunshan et al. in 1980. The typical section is situated in Shiyingliang (Olongbluk Mountain) in Wulan County, Qinghai Province. Upper-middle formation of Quangji Gr.
Synonym: (石英梁组)
Lithology and Thickness
Lower part is composed of red purple ferruginous siltstone, ferruginous silty claystone intercalated with unstable conglomerate and white gray giant-bedded quartzite. Upper part consists of greenish gray basalt, silty shale, gray and grayish black glauconitic siltstone and quartzose sandstone, which is intercalated with two beds of volcanic rock (or pyroclastic rock) and multilayered glauconite and oolitic hematite. Thickness varies from 150 to 395 m.
Relationships and Distribution
Lower contact
Generally, there is occurrence of basal conglomerate, and the basal part overlies disconformably the underlying Kubaimu Fm (Gubaimu Fm)
Upper contact
The top conformably underlies the Hongzaoshan Fm
Regional extent
North-central Qinghai. The Shiyingliang Formation is dominantly distributed in Olongbluk Mountain, Quanji Mountain, Shihui valley and Annanba (in north fringe of Qaidam Basin) in Qinghai Province.
GeoJSON
Fossils
The microclastic rock yields microplants: Trematosphaeridium sp., Protosphaeridium sp., Orygmatosphaeridium cf. rubiginosum, O. sp., Taeniatum crassum, T. sp., Lignum sp., Laminarites sp. etc.
Age
Depositional setting
Additional Information