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
Taipinglinchang Formation
Click to display on map of the Ancient World at:
Taipinglinchang Fm base reconstruction

Taipinglinchang Fm


Period: 
Cretaceous

Age Interval: 
Late Cretaceous, (20) K2t


Province: 
Heilongjiang

Type Locality and Naming

Jiayin Basin. The Taipinglinchang Formation was erected by the Heilongjiang First Regional Geological Survey Team in 1979. The section for the designation is in Taipinglinchang of the Jiayin County of Heilongjiang (130°58′E; 48°51′31″N). [This is the lower-middle formation of Jiayin Gr .]

[Figure: Taipinglinchang Formation at type section in Jiayin, Heilongjiang Province]


Lithology and Thickness

The Taipinglinchang Formation is composed of gray microclastic rocks and oil shale, which is divided into two parts. Lower part is built up by oil shale, mudstone and clayey siltstone, forming a reversed rhythm that is from fine-grained to coarse-grained. Upper part is built up by fine-grained arkose sandstone, siltstone, silty mudstone and mudstone, forming rhythmic interbeds. It is 635.2 m thick.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

The disconformable base of the formation as marked by dark gray schistose oil shale is distinguished from tuffaceous sandstone of the underlying Yongancun Fm.

Upper contact

The disconformable top as marked by siltstone is distinguished from conglomerate of the overlying Yuliangzi Fm.

Regional extent

The present formation occurs along the bank of the Heilong river from the Yongan Village to the Wuyun Town. Around the Yongan Village there crop out the central and middle parts of the formation, which are dominated by sandy mudstone, with oil shale at the base and with sandstone increasing in amount from bottom upward, with marl lenses. It is 155.3 m thick. From the Shuanghe Town to Xiangyang there crops out the upper part of the formation, which is built up by a set of variegated mudstone with sandstone, with grit at the base lying unconformably on the Yanshanian granite. It ranges from 139 to 229 m in thickness. As exposed in the borehole No.2P-shan north of the Sunhao Town, the formation is represented by a set of gray green and black mudstone and sandy mudstone with gravel-bearing sandstone, lying unconformably on the Paleozoic granite, measuring 192 m in thickness.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[128.41,49.48],[129.07,49.23],[129.9,48.71],[129.88,48.46],[129.85,48.17],[130.17,47.87],[130.14,47.68],[129.85,47.56],[129.32,47.54],[128.56,47.74],[127.99,47.92],[127.43,48.18],[126.91,48.4],[126.36,48.84],[126.23,49.29],[126.27,49.56],[126.65,49.73],[127.08,49.56],[127.61,49.5],[128.41,49.48]]]]}}

Fossils

The formation yields floras Trapa? microphylla, Quereuxia angulata, Rhamnites marginatus, Patanus raynolasii, Taxodium sp., Sequoia sp., Metasequoia sp.; sporopollen grains Aquilapollenites sp., Proteacidites sp., Beaupreaidites sp.; ostracods Cypridea perelegana,; estheria Euestheria sp.


Age 


Age Span: 

    Beginning stage: 
Santonian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
84.68

    Ending stage: 
Campanian

    Fraction up in the ending stage: 
0.3

    Ending date (Ma):  
80.21

Depositional setting

It belongs to lacustrine deposition.


Depositional pattern:  


Additional Information


Compiler:  

Wan Xiaoqiao