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Suibin Formation

Suibin Fm


Period: 
Jurassic

Age Interval: 
Upper Jurassic, (TJ13a)


Province: 
Heilongjiang

Type Locality and Naming

It was named by the No. 110 Party of the Northeast China-Inner Mongolian Coal Company in 1992. The naming section is located at about 10 km east of the Shuibin Farm of Suibin County, Heilongjiang Province.

Synonym: (绥滨组)


Lithology and Thickness

It is composed mainly of grey-white medium-, and fine-grained sandstones intercalated with dark-grey siltstone, with a maximum thickness being of 263 m.


Lithology Pattern: 
Fine-grained sandstone


Relationships and Distribution

Lower contact

Its basal part is in an unconformable contact with the underlying late Permian sandstone or the Proterozoic granite. However, regionally, the next older unit is the late Triassic Nanshuangyashan Fm of tuff and tuffaceous sandstone.

Upper contact

Regionally, the schematic strat column indicates the next younger unit as Dongrong Fm

Regional extent

The formation belongs to marine clastic deposits of an early-stage marine invasion, with its distribution being restricted to the Puyang Depression of Suibin County, and with a thickness of about 90-270 m.


GeoJSON

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Fossils

It yields bivalve fossils as represented by Filosina subovalis, Palaconucula makitoensis and Nuculana aff. roederi.


Age 

Schematic stratigraphic column suggests Oxfordian

Age Span: 

    Beginning stage: 
Oxfordian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
161.53

    Ending stage: 
Oxfordian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
154.78

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)