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Tuanbugou Formation

Tuanbugou Fm


Period: 
Devonian

Age Interval: 
D2 (51), Middle Devonian


Province: 
Gansu

Type Locality and Naming

The type section is located at Tangbugou, 18 km northwest of Wenxian County, Gansu. It was named by Zhang Yan in 1961, and Cao Xuanduo formally quoted it in 1990.


Lithology and Thickness

Slate, limestone. This formation is separated from the underlying Shawan Fm by the appearance of shale and calcareous shale intercalated with thin-bedded limestone at a conformable contact. Above that, it is characterized by dark-gray to blackish-gray medium- to thick-bedded micrite limestone, dolomitic-bearing micrite with siliceous nodules, and banded micrite intercalated with thin-bedded limestone and calcareous slate. Its uppermost portion is characterized by thick-bedded to massive limestone with siliceous nodules and banded micrite. The total thickness is 196.4 m.


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

This formation is separated from the underlying Shawan Fm by the appearance of shale and calcareous shale intercalated with thin-bedded limestone at a conformable contact.

Upper contact

The top boundary to the Cakuohe Fm is the top of a thick-bedded limestone with flint nodules (Cao Xuanduo et al., 1990).

Regional extent


GeoJSON

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Fossils

The main fossils are coral Temnophyllum, Hexagonaria, Alveolitella, Natalophyllum, Syringopora, and brachiopods Emanuella, Schizophoria, etc.


Age 

Middle Devonian

Age Span: 

    Beginning stage: 
Givetian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
382.74

    Ending stage: 
Givetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
378.90

Depositional setting

It is interpreted as a carbonate platform facies, because within the limestone are small bedded to hummocky stromatopora reefs.


Depositional pattern:  


Additional Information


Compiler:  

(Cao Xuanduo)