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Gongguan Formation

Gongguan Fm


Period: 
Devonian

Age Interval: 
D1-2 (45-47), Lower Devonian (South) to Middle Devonian (North)


Province: 
Shaanxi, Gansu

Type Locality and Naming

The type section is located at Xichaliangding—Xujiacao, Luohe Township, Xunyang County, Shaanxi Province. It was named by No 1 Shaanxi Geological Team in 1964 and was published by “Regional Stratigraphical Scale of Central-Southern China” in 1974.


Lithology and Thickness

Dolomite. It is dolomitic rocks. The total thickness is 549.8 m . Lower part composed of gray and dark-gray medium-bedded micritic limestone and fine-grained dolomite intercalated with dolomitic slate. Upper part composed of gray to light-gray medium-bedded sandy dolomite intercalated with clayey dolomite.

In Gongguan area, this formation is composed of algal dolomite and stromatolite-bearing dolomite, with trough and tabular cross-bedding in the Lower part, with climbing-ripple lamination, lenticular bedding and flaser bedding in the Middle part, and with exposure marks such as bird's-eyes, mutlion structures, drying cracks, etc. in the Upper part.


Lithology Pattern: 
Dolomitic limestone


Relationships and Distribution

Lower contact

This formation overlies conformably on the Xichahe Fm.

Upper contact

Conformably overlain by the Shijiagou Fm.

Regional extent

The formation is distributed in the area of Xunyang and Shanyany counties, along the western margin of Wudang Old Land.


GeoJSON

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Fossils

In the upper part, it yields ostracods Paramoelleritia subtrapezoidalis; gastropods Murchisonia cf. loxomemoides; and Stromatopora Amphipora


Age 


Age Span: 

    Beginning stage: 
Emsian

    Fraction up in beginning stage: 
0.1

    Beginning date (Ma): 
408.89

    Ending stage: 
Emsian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
394.30

Depositional setting

It is interpreted as a tidal flat to lagoon facies deposit deposited within a marine transgression.


Depositional pattern:  


Additional Information

In Gongguan-Shuanghe area, it may reach up to 550~689 m in thickness, and belongs to the Lower Devonian. But was deposited within a marine transgression from south to north, therefore in Nankuanping--Shanyang, the thickness reduces down to 47~160 m and the age correspondingly goes up to Middle Devonian.


Compiler:  

(Cao Xuanduo)