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Shangdaminshan Formation
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Shangdaminshan Fm base reconstruction

Shangdaminshan Fm


Period: 
Devonian

Age Interval: 
D32 (5), Famennian (latest Devonian)


Province: 
Heilongjiang

Type Locality and Naming

The type section is located east of Daminshan Hill, south of Zadunhe River of Mianduhe Town of Da Hinngan Ling, Heilongjiang Province. It was named by Ning Qisen et al. in 1958


Lithology and Thickness

Tuff. The Shangdaminshan Formation is characterized by grayish-green andesite porphyry tuff and tuffaceous sandstone intercalated with thin beds or lenses of purplish-red limestone, and has tuffaceous conglomerate and breccia at the base. In the type area, this formation is more than 199 m.


Lithology Pattern: 
Volcanic_ash


Relationships and Distribution

Lower contact

In the type area, this formation rests conformably on the Xiadaminshan Fm volcanic ash

Upper contact

In the type area, this formation is overlain by volcanics of unknown age.

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[120.68,50.36],[120.86,48.89],[121.92,49.14],[122.78,50.37],[121.66,51.31],[120.68,50.36]]]]}}

Fossils

The limestone includes ammonoids of the Cheiloceras subpartitum Zone and Platyclymenua walcotti Zone, and corals Nalivkinella daminshanensis.


Age 

Famennian (latest Devonian)

Age Span: 
S

    Beginning stage: 
Famennian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
371.10

    Ending stage: 
Famennian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
359.30

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

(Hou Hongfei)