Dakui Fm
Type Locality and Naming
The type section is the core taken from the hole near Village Dakui in the northern segment of prospecting line No. VI of Damao phosphate deposit in Sanya, Hainan. The Dakui Fm in derived from the Dakui Gr proposed by Guangdong Party of Regional Geological Survey in 1964. Ge Meiyu et al. (1983) renamed the Dakui Gr the Dakui Fm.
Synonym: (大葵组)
Lithology and Thickness
In the type area, the Dakui Fm is divided into two parts. Lower part is composed of light gray, bluish gray inequigranular quartz sandstone. Upper part is represented by gray to dark gray thick-bedded limestone.
Relationships and Distribution
Lower contact
Disconformably overlies the Damao Fm of middle Cambrian
Upper contact
Conformably overlain by the Yahua Fm
Regional extent
GeoJSON
Fossils
It bears minor pebbles and clasts of brachiopod and micropaleoplants such as Leiominuscula sp., Archaeodiscina sp.in the lower part, and yields conodont Pariostodus parallelus, Serratognathus bilobatus, Scolopodus cf. rex, S. cf. rex huolianzhaiensis, Oepikodus cf. ommunis, cf. Scolopodus eburnus and Acontidus? linxiensis in the upper part.
Age
Depositional setting
Additional Information