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YangshanHenan Formation

YangshanHenan Fm


Period: 
Carboniferous

Age Interval: 
C21 (27), middle-late Early Carboniferous


Province: 
Henan

Type Locality and Naming

The type section is located at Wushanglou on the west slope of Dayangshan (Mt.), about 10 km southeast of Nanfangji, Gushi County, Henan. It was named by Nie Zongsheng et al. in 1959.

[NOTE: Carboniferous Lexicon Column 44 (Shaanxi collision belt) had a Yangshan Fm between Yaxi Fm and Xianyao Fm, which has a type section at Yangshan (unlike this one) => therefore, named these as "YangshanHenan" and "YangshanShaanxi" (maybe Chinese characters are different for these?)]


Lithology and Thickness

Sandstone and Coal. Dominated by interbeds of quartz conglomerate and sandstone, intercalated with mudstone and coal seams, totaling 655−855 m thick. The coal seams in the formation are unstable.


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

Conformable contact with the underlying Dayangshan Fm

Upper contact

Disconformable contact with the overlying Miaochong Fm

Regional extent

Mainly distributed along the Pichong coal mine, Wujianshan, Laoyingzi, Dayangshan and the Yangshan coal mine


GeoJSON

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Fossils

Contains abundant Plants Rhodea hsianghsiangensis, Bothrodendron flabellatum, Triphyllopteris sp., Lepidostrobophyllum cf. lanceolatatum, Sublepidodendron mirabile, Cardiopteridium spetsbergense, Eusphenopteris cf. scribanii, Adiantites cf. gothani, Lepidodendron aff. Aolungpylukense, etc.


Age 

middle-late Early Carboniferous

Age Span: 

    Beginning stage: 
Visean

    Fraction up in beginning stage: 
0.8

    Beginning date (Ma): 
333.62

    Ending stage: 
Serpukhovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
323.40

Depositional setting

It is interpreted as swamp coal-bearing deposits in a gray molasse deposit


Depositional pattern:  


Additional Information


Compiler:  

Wang Rennong