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Huanggang Formation

Huanggang Fm


Period: 
Neogene

Age Interval: 
Late Miocene (Messinian), N1 , (23a)


Province: 
Jiangsu

Type Locality and Naming

Its type section is located at Huanggang (E118°48′, N32°29′), southeast of Maji town, Liuhe County, 20 km north of Nanjing City, Jiangsu Province. It was named by Bi et al. (1977).

Synonym: Bureau of Geology and Mineral Resources of Jiangsu Province (BGMRJ(Jiangsu)P) (1997) assigned the Huanggang Fm as a synonym of the Yuhuati Fm and correlated the former to the middle part of the latter. Gao et al. (2014a) treated the FangshanBasalt Fm, the Lingyanshan Fm, and the Guiwu Fm as synonyms of the Huanggang Fm


Lithology and Thickness

The Huanggang Fm is divided into two members. Lower member consists of greyish-cyan or greyish-green mudstones, muddy dolomites, and gravels interbedded with olivine basalts. Upper member is characterized by brick-red, brownish-yellow, greyish-green, brownish-grey, and greyish-yellow gravels, sandstones, siltstones, and deep red tuffaceous gravels with thin basalt layers. It contains mammalian fossils. Its thickness is in range of 15~70 m.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

In the type section, the Huanggang Fm disconformably contacts with the underlying XiaopanshanBasalt Fm. Regionally, the next older unit is the Liuhe Fm.

Upper contact

In the type section, the Huanggang Fm disconformably is overlain by the PingshanBasalt Fm (similar to JianshanBasalt Fm ?)

Regional extent

This formation is widely distributed to region ranging Jiangning, Liuhe, Xiaopanshan, Fangshan, Renjiaju, Huanggang, Chenxiangying, and Xuyi, Jiangsu Province.


GeoJSON

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Fossils

Mammals: Hipparion cf. H. platyodus, “Diceratherium” cf. D. minus, ?Pliomastodon cf. P. matthewi, Giraffidae indet., Cervidae indet.. (Bi et al., 1977)


Age 

The basalts in the Huanggang Fm have a magnetic dating that is in range of about 10~12 Ma. The Huanggang Fauna can be correlated to the Baode Fauna of Shanxi Province in sharing Hipparion, Diceratherium, and Pliomastodon. The age of the Huanggang Fm is in late Miocene..

Age Span: 

    Beginning stage: 
Tortonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
11.63

    Ending stage: 
Tortonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
7.25

Depositional setting

It is interpreted as a river environment.


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Sukuan Hou, J.Z. Qigao, Q. Li, Q.Q. Shi, B.Y. Sun, S.Q. Wang, F.X. Wu