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Yamansu Formation

Yamansu Fm


Period: 
Carboniferous

Age Interval: 
C21 (8a), middle-late Early Carboniferous


Province: 
Xinjiang

Type Locality and Naming

The type section is located at Dagou, Yamansu District, Xinjiang. It was named by Zhang Quanhui in 1958.


Lithology and Thickness

Limestone, Sandstone and Volcaniclastics. A suite of neritic terrigenous clastic rock, carbonate rock and pyroclastic rock. Dominantly dark-gray to gray thick-bedded limestone, bioclastic limestone, reef limestone, oolitic limestone, sandy limestone, clayey limestone, gray-green thick-bedded calcareous sandstone, greywacke-cobblestone, pebbly grit, calcareous siltstone, light-gray-green thin-bedded tuff, purple-gray tuff, tuffaceous sandstone and siltstone, occasionally intercalated with lava. Exposed thickness 2237 m. Westward to Aqi Mt., lavas increase, containing fusulinid Eostaffella sp., and regionally from east to west carbonate rocks decrease while volcanic rocks increase, 1826−2887 m in thickness.


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

Conformable contact with the underlying Xiaorequanzi Fm

Upper contact

Disconformable contact with the overlying Dikaner Fm

Regional extent

Distributed at Qoltag, extending nearly E-W.


GeoJSON

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Fossils

Contains abundant Corals Yuanophyllum sp., Clisiophyllum sp., Gangamophyllum sp., Lithostrotion sp., Palaeosmilia sp., Hexaphyllia sp., Rotiphyllum sp., Dibunophyllum sp. and Cystodendropora sp.; Brachiopods Gigantoproductus sp., Striatifera striata, Linoproductus sp. and Chonetipustula sp.; Ammonoids Platygoniatites molaris, Proshumardites sp., Irinoceras sp., Dombarites paratectus and Syngastrioceras sp., as well as gastropods, bivalves, bryozoans, algae, etc.


Age 

middle-late Early Carboniferous

Age Span: 

    Beginning stage: 
Visean

    Fraction up in beginning stage: 
0.2

    Beginning date (Ma): 
343.45

    Ending stage: 
Serpukhovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
323.40

Depositional setting

It is interpreted as a neritic facies with volcanism.


Depositional pattern:  


Additional Information


Compiler:  

Zhang Zixin