Quanji Gr
Type Locality and Naming
North-central Qinghai. The Quanji Gr was named by the No. 632 Team of Petroleum Reconnaissance Survey of Qinghai Bureau of Geology in 1956 and formally published by Wang Yunshan in 1980. The typical section is situated in Quanji Mountain in northern fringe of Qaidam Basin (Daqaidam), Qinghai Province.
Synonym: (全吉群)
Lithology and Thickness
Lower part is composed of conglomerate and pebbly sandstone (Mahuanggou Fm), followed by rhythmic sandstone (Kubaimu Fm), shale, quartzite and basalt (Shiyingliang Fm) and carbonate rock bearing stromatolites and algae (Hongzaoshan Fm). The thickness varies from 778.6 to 2830.2 m. See individual formations for details.
[Figure: The Quanji Group in the Quanji Mts in Qinghai Province (section and field photos by Kuang Hongwei)]
Relationships and Distribution
Lower contact
The lower part rests unconformably on the Mesoproterozoic Dakendaban Gr (Ch).
Upper contact
The upper part is conformably overlain by the "Lower Cambrian" Heitupo Fm (Xiaogaolu Gr) – which is now considered a mid-Mesoproterozoic (middle Ectasian)
Regional extent
North-central Qinghai. The Quanji Gr is mainly distributed in Olongbluk Mountain, Shihuigou, Quanji Mountain and Datouyang valley in northern fringe of Qaidam Basin, Qinghai Province
GeoJSON
Fossils
Age
Depositional setting
Additional Information