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Tangjiatun Formation

Tangjiatun Fm


Period: 
Carboniferous

Age Interval: 
C12 (13b), early Late Carboniferous


Province: 
Heilongjiang

Type Locality and Naming

The type section is located at Beishan, Tangjiatun, Acheng County, Heilongjiang. It was named by Zheng Guangyuan et al. in 1961.


Lithology and Thickness

Volcaniclastics. The formation is a stratum dominated by a suite of acid metamorphic volcanic rocks, with more sedimentary intercalations in the lower part than in the upper part. Lower part consists of yellow-brown and gray-black schistosed acid and intermediate-acid tuffaceous lava intercalated with schistosed gray-green tuffaceous sandstone, siltstone and slate. Upper part is dominated by rhyolitic tuffaceous lava intercalated with tuff and schistosed siltstone. Thickness >1211 m. 685 m thick at Beishan of Sunjiagong, Binxian County. Lava flows are not well developed, and are mostly tuffaceous lavas. From north to south the thickness increases and lava flows decrease.


Lithology Pattern: 
Volcanics


Relationships and Distribution

Lower contact

Uncertain relationships with the underlying strata (Chaergelahe Fm)

Upper contact

Uncertain relationships with the overlying strata (Yangmugang Fm)

Regional extent

Distributed in the areas such as Sunjiagang of Binxian County, Tangjiatun and Yagou of Acheng City as well as Yangmudingzi of Wuchang County.


GeoJSON

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Fossils

Plant Paracalamites sp. has been collected from the tuffaceous silty slate intercalation of rhyolitic tuffaceous lava at Beishan, Tangjiatun, Acheng County.


Age 

Age of 305 Ma according to Rb-Sr isotope dating => early Late Carboniferous

Age Span: 

    Beginning stage: 
Bashkirian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
323.40

    Ending stage: 
Moscovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
307.02

Depositional setting

It is interpreted as a


Depositional pattern:  


Additional Information


Compiler:  

Liu Fa