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Niugundang Formation

Niugundang Fm


Period: 
Jurassic

Age Interval: 
Late Jurassic, (TJ77)


Province: 
Sichuan

Type Locality and Naming

It was named by No. 1 Regional Survey Party under the Geological Bureau of Sichuan Province in 1966, and was first cited publicly by the Compiling Group for the Regional Stratigraphic Chart of Sichuan Province. The naming section is located in the area of Xincun Village of Changxin Township till Guangou Gully, Huidong County, Sichuan Province.

Synonym: (牛滚凼组)


Lithology and Thickness

Composed largely of bright-red and brown-red mudstones and calcareous mudstones, with its top part being intercalated with grey and purple thin-bedded-thick-bedded marls, with the mudstones often containing scolites, and with a thickness commonly of 300-500 m.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

It is in a conformable contact with the underlying Xincun Fm

Upper contact

It is in a conformable contact with the overlying Guangou Fm

Regional extent

The formation is distributed in the areas of Huidong, Huili and Xichang of southwestern Sichuan. Its lithology in various regions is comparatively stable, being represented entirely by bright-red mudstone, and thus being known as the “Wine-Red Strata”.


GeoJSON

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Fossils

It yields Ostracoda fossils as represented by Darwinula sarytirmenensis and D. impudica, as well as bivalve and Gastropoda fossils.


Age 

Schematic strat column in previous "red Chinese Lexicon" had implied that the Niugundang Fm spanned the early-Late Jurassic.

Age Span: 

    Beginning stage: 
Oxfordian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
161.53

    Ending stage: 
Kimmeridgian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
152.01

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)