Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Hongshan Formation

Hongshan Fm


Period: 
Permian

Age Interval: 
P2 - P3 (18), middle to late Permian


Province: 
Heilongjiang

Type Locality and Naming

The type section is located at 1 km to the northwest of the Hongshan Mt., Yichun City, Heilongjiang Province; and the reference section is situated at Shangganling Ridge of Yichun City. It was named by Zhang Hairi et al., of the 1st Regional Geological Survey Party under the Geological Bureau of Heilongjiang Province in 1971.


Lithology and Thickness

Sandstone. It can be divided into three parts: Lower part is composed of grey-white coarse-, and fine-grained sandstones, intercalated with black slate and carbonaceous slate, with a thickness of 181 m. Middle part is composed of alternation of beds of pebble-bearing-coarse-grained sandstone, siltstone, fine-grained sandstone and slate, with a thickness of 323 m. Upper part is composed of grey-black and light-grey fine-grained sandstone, siltstone and sandy slate, intercalated with pebble-bearing coarse-grained sandstone, with a thickness of over 195 m. Its total thickness is 699 m.


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

Uncertain contact with the underlying Wudaoling Fm.

Upper contact

Regional extent

Distributed in the areas of Shangganling Ridge, Hongshan Mt., Weiguo, Wuxing and Wuying to the north of Yichun City.


GeoJSON

null

Fossils

Plant fossils (phytolites) such as the Comia yichunensis, Lobatannularia multifolia, Callipteris zeilleri, Pecopteris, Noeggerathiopsis angustifolia, Compsopteris, Supaia, Rhipidopsis and Taeniopteris, with the members of the Angara flora being predominant. Jin Jianhua et al. (1992) would think that the plant assemblage of the Lower Member of the Sanjiaoshan Fm is more or less similar to that of the Hongshan Fm.


Age 

Assigned as middle or upper Permian

Age Span: 

    Beginning stage: 
Wuchiapingian

    Fraction up in beginning stage: 
0.25

    Beginning date (Ma): 
258.22

    Ending stage: 
Wuchiapingian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
254.24

Depositional setting

It is interpreted as river-lake clastics.


Depositional pattern:  


Additional Information


Compiler:  

Li Li