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Gerong Formation
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Gerong Fm base reconstruction

Gerong Fm


Period: 
Devonian

Age Interval: 
D1 (33), Early Devonian


Province: 
Sichuan

Type Locality and Naming

The type section is located at the Cow Farm of Zongza in Batang County, westernmost Sichuan Province near border with Tibet. It was named by Sichuan No 3 Team of Regional Geological Survey in 1977 and was published by Sichuan Compiling Group for Regional Stratigraphical Scale in 1978.


Lithology and Thickness

Dolomite. It is a set of carbonate rock and is mainly composed of light-gray to grayish-white thick-bedded dolomite and dolomitic limestone, partly intercalated with thin- to medium-bedded quartz sandstone. It is 124 m in thickness.


Lithology Pattern: 
Dolomite


Relationships and Distribution

Lower contact

Conformably on the grayish-white medium-bedded crystalline limestone of the Yiongren Fm of the Upper Silurian.

Upper contact

Conformably overlain by the quartz sandstone at base of the Qiongcuo Fm.

Regional extent

The formation is distributed at Zongza of Batang County and in Dêrong County. Trending to Secang of Zhongdian (now Shangri-La) County, Yunnan Province, the facies changes into interbeds of gray sandy slate with dark-gray thick-bedded limestone, which contain abundant brachiopods and corals fossils.


GeoJSON

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Fossils

It yields corals Tryplasma, Lyrielasma, Favosites.


Age 

Early Devonian

Age Span: 
S

    Beginning stage: 
Lochkovian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
419.00

    Ending stage: 
Emsian

    Fraction up in the ending stage: 
0.8

    Ending date (Ma):  
397.54

Depositional setting

It is interpreted as a lagoon facies deposit.


Depositional pattern:  


Additional Information


Compiler:  

(Xian Siyuan)