Wenduraobaote Fm
Type Locality and Naming
The type section is located in north of Wenduraobaote and Aobaotinghundi, the west hill of east Wuchumuqinqi, Inner Mongolia Autonomous Region. It was named by Inner Mongolia Team of Regional Geological survey in 1973 during mapping the “East Wuchumuqinqi Geological Map (scale is 1:20000)”.
Synonym: Wenduraobaote Gr (Group)
Lithology and Thickness
Tuff. The lithology is complex and is mainly composed of tuff, crystal lithoclastic tuff, siltstone, feldspathic quartz sandstone and slate. Characteristic markers are the content of thin beds or lenses of limestone that are distributed very steady along strike. Limestone beds can attain 30 m in thickness and commonly are lenses.
The outcropped thickness can reach 1228 m.
Relationships and Distribution
Lower contact
Thin beds or lenses of limestone make it easy to differentiate this formation from the conformably underlying Aobaotinghundi Fm.
Upper contact
Regionally, unconformably overlain by late-Late Devonian tuffs of Honggermiao Fm; or locally conformably overlain by siltstone of Taerbaogete Fm.
Regional extent
GeoJSON
Fossils
Characteristic markers are the content of thin beds or lenses of limestone that are distributed very steady along strike and contain abundant Tetracoralla and brachiopods fossils.
The formation yields brachiopods Tridensilis app, "Paraspirifer" sp., Narelophyllum sp., Cylindrophyllum sp., Keriophyllum sp.; and Stromatopora Anostylostroma sp., Trupebostroma sp., etc.
Age
Depositional setting
Additional Information