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Shuigoukou Formation

Shuigoukou Fm


Period: 
Cambrian

Age Interval: 
Probably Nangaoan through Duyunian (mid-Cambrian). (73)


Province: 
Shaanxi

Type Locality and Naming

No type section is assigned when Lu (1962) published the unit. An auxiliary section, Yuejiaping section, was proposed by Xiang (1981d) as representative section of the formation. This section lies at side of the highway between Yuejiaping and Wangjiadian villages, 6.5 km south of Xianghe Town, or about 32 km south of the seat of Shangnan County, Shangluo City, southeastern Shaanxi Province. (110°53’26” E, 33°14’50” N). In the auxiliary section, the Shuigoukou Formation is 47.3 m thick.

Synonym: (水沟口组)


Lithology and Thickness

The Shuigoukou Formation is a sequence with siliceous rocks in lower part and carbonate rocks in middle and upper parts. Lower part, mainly consists of black, dark grey, thin-bedded siliceous rack, carbonaceous siliceous rack and yellowish grey and black aluminous shale with phosphoric nodules; the middle and upper parts consists of multi-colored (dark grey, greyish purple, light grey, greyish white) limestone, argillaceous limestone, and dolomitic limestone.


Lithology Pattern: 
Siliceous limestone


Relationships and Distribution

Lower contact

The Shuigoukou Fm rests disconformably on Tongying Fm. The lower boundary of the formation is marked by the disconformable plane.

Upper contact

It is conformably overlain by Yuejiaping Fm, east of Shanyang Town, and by Shihwengtzu Fm, west of Shanyang Town. The upper boundary is defined by the appearance of thick-bedded dolomite at the base of the Shihwengtzu Fm or the appearance of purple dolomite at the base of of Yuejiaping Fm.

Regional extent

The Shuigoukou Formation is exposed in the Jiangbei Slope Area of South China Region, restricted to southeastern Shaanxi Province (Shangnan, Shanyang, Zhen’an, and Ningshan counties). The thickness of the formation varies from 19 to 60 m.


GeoJSON

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Fossils

The lower part of the Shuigoukou Formation yields hylolithid Hyolithes sp.; the middle-upper part of the formation yields trilobites Kootenia yui., Palaeolenus quadratus., Redlichia murakamii, and R. chinensis and Shifangia yefanggouensis.


Age 

Probably Nangaoan through Duyunian. (Mid-Cambrian)

Age Span: 

    Beginning stage: 
Cambrian Stage 3

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
521.00

    Ending stage: 
Cambrian Stage 4

    Fraction up in the ending stage: 
0.75

    Ending date (Ma):  
510.38

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Peng Shanchi