Amunik Fm
Type Locality and Naming
The type section is located at Amunik Mt., southeast of Xitieshan and southwest of Delingha, in the northern margin of Qaidam Basin, Qinghai Province. It was named by Qinghai No 1 Team of Regional Geological Survey in 1976.
Lithology and Thickness
Sandstone, conglomerate. The formation is mainly characterized by purple, grayish-purple, gray, yellowish-pink arkosic quartzose sandstone and silty mudstone. At the bottom is a bed of purple conglomerate about 2 m thick. The composition of the conglomerate is mainly chert, volcanic rock and limestone, with the pebbles being 2-4 cm in diameter, angular to subangular in shape and cemented with sands. In Amunik section, the formation is 116 m in thickness.
Relationships and Distribution
Lower contact
Disconformable contact with the underlying Maoniushan Fm.
Upper contact
Conformable or disconformable contact to the overlying Chengqianggou Fm of Lower Carboniferous.
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Additional Information