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Guanshanpo Formation
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Guanshanpo Fm base reconstruction

Guanshanpo Fm


Period: 
Devonian

Age Interval: 
D1 (70), Early Devonian


Province: 
Sichuan

Type Locality and Naming

The Guanshanpo Fm is the uppermost formation in the Pingyipu Gr. The type section is located between northwest of Ganxi Village and the 71 km milestone of the Mianping road in Beichuan County, Sichuan Province. It was named by Hou Hongfei, Wan Zhengquan et al. in 1988.


Lithology and Thickness

Sandstone. It is dominated by gray to light-gray medium-bedded fine-grained quartz sandstone intercalated with greywacke. It is 242 m in thickness.


Lithology Pattern: 
Fine-grained sandstone


Relationships and Distribution

Lower contact

It rests in a conformable contact with the underlying Guanyinmiao Fm

Upper contact

It is in a conformable contact with the overlying Bailiuping Fm

Regional extent

The formation is mainly developed at Ganxi of Beichuan County and also in Pingwu County; and it thickness reduces at Yanmenba in Jiangyou County, at the southeast limb of Tangwangzhai syncline.


GeoJSON

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Fossils

The lower part yields fish fossils Macropetalichthys and Arthrodira; the middle part yields bivalve, ostracods, inarticulate brachiopods, plant and spore fossils; and trace fossils are developed in the upper part. In Ganxi section of Beichuan County, this formation yields fish fossils Chuanbeiolepis jiangyouensis, Yunlongolepis ligui, Parapetallichthys minor and fragments of Arthrodira, as well as bivalves, plants.


Age 

Early Devonian

Age Span: 
S

    Beginning stage: 
Pragian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
412.40

    Ending stage: 
Pragian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
411.46

Depositional setting

Dleta


Depositional pattern:  


Additional Information

.


Compiler:  

(Wang Shitao)