Taowan Fm
Type Locality and Naming
North Qinling Mts (west Henan). The Taowan Fm was named by Yan Lianquan in 1959. The type section is located at Taowan Town, Luanchuan County, Henan Province.
Synonym:
Lithology and Thickness
The Taowan Fm consists of two parts. Lower part is the Mugou Member (although some geologists consider it as the upper part), which consists mainly of gray, gray-white thick- to medium-bedded marble, interbedded with carbonaceous phyllite with hematite and biotite-sericite quartz schist. Upper part, the Fengmaimiao Member, is composed of sericite dolomite marble, thin-bedded banded marble, quartz phyllite, sericite phyllite, and locally phyllite interbedded with marble. The Taowan Formation is 930-2000 m thick.
Relationships and Distribution
Lower contact
The bottom boundary is unexposed or is an unconformable with the underlying Kuanping Gr (Mesoproterozoic)
Upper contact
The Taowan Fm is unconformably covered by the calcareous conglomerate of Sanchakou Fm (Ediacaran)
Regional extent
North Qinling Mts (west Henan-southeast Shaanxi). At present, the Taowan Formation is tectonically restricted to the north of Tieluzi-Luanchuan fault. It is widely distributed from Luonan, Lanqiao Town in Lantian, Shaanxi Province to Lushi, and eastwards to Miaozi Town, Luanchuan, Henan Province, trending E-W over 230 km.
GeoJSON
Fossils
Microplants: Lignum nematoideum, Polyporata microporosa, Laminarites sp.? Triangumorpha sp., Trematosphaeridium holtedahlii, Trachy- sphaeridium sp., Taeniatum crassum, Leiopsophosphaera sp., Margominuscula sp. etc.
Age
Depositional setting
Additional Information