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Xiertala Formation

Xiertala Fm


Period: 
Carboniferous

Age Interval: 
C21 (14), late Early Carboniferous


Province: 
Inner Mongolia

Type Locality and Naming

The type section is in the borehole ZK105, about 40 km east of Hailar City, Inner Mongolia. It was named by the No. 6 Geological Party of Heilongjiang in 1976.


Lithology and Thickness

Limestone, Claystone and Sandstone. A suite of marine carbonate and clastic rocks. The Bottom is of gray-white to purple marbleized limestone; containing brachiopods and corals; the lower and middle parts consist of black shale, gray-black micritic limestone, calcareous sandstone and siltstone interbeds; the upper part consists of gray calcareous grit, fine-grained sandstone, siltstone, etc. intercalated with limestone. Exposed thickness 211 m.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

Conformable contact with the underlying Moergenhe Fm volcaniclastics

Upper contact

Unknown: The top is covered by Quaternary stratum in type section. Regionally, the next higher unit is the Xiertala Fm limestone.

Regional extent

Distributed in such areas as the Xiertala Fe-Zn mining district, southern Ewenki Autonomous Banner, Wunuer of Yakeshi City, Lingbei Railway Station and Shangkuli of the Ergun Right Banner.


GeoJSON

null

Fossils

Brachiopod Megachonetes-Davidsonia assemblage, including Fluctuaria undata, Brachythyris cf. ovalis, Syringothyris cf. cuspidata, Neospirifen liangchouensis, Striatifera aff. striata, Linoproductus tenuistriatus, etc. Corals Zaphrentites sp., Zaphrentoides sp., Hexaphyllia sp., Rotiphyllum sp., etc.


Age 

late Early Carboniferous

Age Span: 

    Beginning stage: 
Visean

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
346.73

    Ending stage: 
Visean

    Fraction up in the ending stage: 
0.8

    Ending date (Ma):  
333.62

Depositional setting

It is interpreted as marine carbonate and clastics.


Depositional pattern:  


Additional Information


Compiler:  

Li Wenguo