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Dingqing Formation

Dingqing Fm


Period: 
Paleogene, Neogene

Age Interval: 
Oligocene-Miocene, E3-N1, (8c)


Province: 
Xizang (Tibet)

Type Locality and Naming

Heihe Squadron of Qinghai Petroleum Survey Brigade named the Dingqing Layer. The Fourth Geological Brigade of Tibet Geological Bureau introduced and renamed the Dingqinghu formation in 1978.

Synonyms: The Dingqing Formation synonymous with the Dingqing Gr, the Dingqinghu Fm, the Qingshi Gr (Qingshi Fm).


Lithology and Thickness

The Dingqinghu Formation comprises purplish-red and greyish-green clastic shale and tuff interbedded with oil shale and marl. The thickness of the Dingqing Formation ranges from 300-1100m.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

The Dingqinghu Formation unconformably overlies the Niubao Fm.

Upper contact

Upper boundary is unobservable. China Lexicon strat chart is confusing here; and usage seems very broad through northern Tibet-Qinghai?

Regional extent


GeoJSON

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Fossils

The Dingqinghu Formation contains fossils of Ostracodas (Cyprinotus, Candona, Ilyocypris), Charophtyes (Charites sadleri), Pollen, Insect, Cyprinid fish (Plesioschizothorax macrocephalus), Mammal (Plesiaceratherium).


Age 

T. Deng et al. (2019, Neogene chapter of China Integrated Stratigraphy and Timescale) indicates upward span to earliest Langhian.

Age Span: 

    Beginning stage: 
Priabonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
37.71

    Ending stage: 
Langhian

    Fraction up in the ending stage: 
0.2

    Ending date (Ma):  
15.56

Depositional setting

Lacustrine deposit facies.


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Sukuan Hou, J.Z. Qigao, Q. Li, Q.Q. Shi, B.Y. Sun, S.Q. Wang, F.X. Wu