Yaxicuo Fm
Type Locality and Naming
Guo Gengcheng named a sequence of carbonate-dominated lacustrine deposits the Yaxicuo Formation in 1989. Its age is Oligocene. In 1994 the Qinghai Bureau of Geology and Mineral Resources renamed it the Yaxicuo Formation and assigned its age to Eocene–Oligocene. The naming section is located at Aburi’ajiazai, Golmud City, Qinghai.
Lithology and Thickness
Lithologically grayish white, thin- to medium-bedded, dolomitic limestone and bioclastic limestone with purplish red sandstone and lime mudstone. The thickness is 230–980 m.
Relationships and Distribution
Lower contact
Its boundary with the underlying Paleogene Tuotuohe Fm is marked by the appearance of limestone.
Upper contact
Its boundary with the overlying Wudaoliang Fm is marked by the appearance of gypsum.
Regional extent
The formation is mainly distributed in the Tuotuo River, Qumar River and Hoh Xil.
GeoJSON
Fossils
The formation contains the ostracods Eucypris and Candoniella, the gastropods Valvata and the charophytes Obtusochara.
Age
Depositional setting
Additional Information