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Huanggexi Formation

Huanggexi Fm


Period: 
Silurian

Age Interval: 
the Aeronian of Llandovery (S1), (48)


Province: 
Yunnan

Type Locality and Naming

The formation was established by the Second Regional Geological Survey of Yunnan Province in 1976. The type section is located in the Huanggexi section, Daguan County, Yunnan Province. Coordinate: 103°52′21″E, 27°50′N. The formation and the overlying Sifengya Fm were treated as the Huanggexi Member and Sifengya Member, respectively, of the Daguan Fm by Rong (1998). Since the distinctive feature of red beds is developed in the overlying strata, the authors agree with the Bureau of Geology and Mineral Resources of Yunnan Province (2008) to treat the former Huanggexi Member and Sifengya Member as the independent formations.

Synonym: (黄葛溪组)


Lithology and Thickness

Lower part of the formation is composed by dark gray, gray thick-bedded limestone and lenticulated limestone; Upper part is composed of gray white, light gray dolomitic quartz silt-fine sandstone intercalated with argillaceous limestone and mudstone.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

The formation is conformably contacted with the underlying Xintan Fm; or the Longmaxi Fm

Upper contact

The formation is conformably contacted with the overlying Sifengya Fm

Regional extent

The formation, 153.9 m in thickness at the type section, is exposed in the area of Zhenxiong County and Weixin County, Northeast of Yunnan Province.


GeoJSON

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Fossils

The formation bears graptolites Glyptograptus, Climacograptus, Orthograptus; trilobite Meitanilaenus, Kosovopeltis, Encrinuroides;brachiopods Zygospiraella, Beitaia, Isorthis and coral Ketophyllum, which are equivalent to part of the graptolite Monograptus sedgwickii zone. The middle and upper parts yield corals Favosites, Palaeofavosites, Halysites, Heliolites, Orthophyllum, Cystiphyllum, Pycnactis, Brachyelasma etc.; brachiopod Zygospiraella, trilobite Songkania; gastropods Loxonema, Discordochilus; which are equivalent to the upper part of the graptolite M. sedgwickii zone.


Age 

Consequently, the age of the formation belongs to Aeronian of Llandovery.

Age Span: 

    Beginning stage: 
Aeronian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
439.73

    Ending stage: 
Telychian

    Fraction up in the ending stage: 
0.1

    Ending date (Ma):  
438.02

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng