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Gudaoling Formation

Gudaoling Fm


Period: 
Devonian

Age Interval: 
D31 (44), Frasnian (early Late Devonian)


Province: 
Shaanxi

Type Locality and Naming

The type section is located near Gudaoling on the border between Zhashui and Zhen’an counties, Shaanxi Province. It was named by Zhao Yazeng and Huang Jiqing in 1931.


Lithology and Thickness

Conglomerate, limestone. The lithology is characterized by a Basal 9.2-m-thick conglomerate and sandy conglomerate intercalated with sandy slate; Lower part of clayey limestone and bioclastic micrite. Upper part of clayey banded limestone and thick-bedded crystalline limestone intercalated with calcareous slate and with some reef limestone breccia seen in the topmost part. The thickness is 412 to 767 m in total.


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

It overlies disconformably on the Shiping Fm of the Middle Devonian.

Upper contact

Disconformably overlain by the Gedasi Fm flysch deposits.

Regional extent


GeoJSON

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Fossils

In the lower part, it yields brachiopods Tenticospirifer, Cyrtospirifer; coral Disphyllum; and conodonts Ancyrodella rotundiloba, Palmatolepis hassi.


Age 

Frasnian (early Late Devonian)

Age Span: 

    Beginning stage: 
Frasnian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
378.90

    Ending stage: 
Frasnian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
371.10

Depositional setting

It is interpreted as a submerged fan changing upward into a biohermal facies.


Depositional pattern:  


Additional Information


Compiler:  

(Cao Xuanduo)