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Jidike Formation

Jidike Fm


Period: 
Paleogene, Neogene

Age Interval: 
Oligocene (? Rupelian to Chattian), E3, (4a)


Province: 
Xinjiang

Type Locality and Naming

Kuqa Depression, NW Tarim The type section is located at the south wing of the Jidike anticline (E83°29′, N42°07′), Kuche City, northern Tarim Basin in Xinjiang. It was formally named by the Regional Stratigraphic Chart Editorial Group of Xinjiang Uygur Autonomous Region (RSCEGXUAR) (1981).

Synonym: Gao et al. (2014a) treated the Qiulitake Gr and the Yanshuigou Fm named by the RSCEGXUAR (1981) as synonyms of the Jidike Fm.


Lithology and Thickness

The Jidike Fm is characterized by a series of brownish-red sandy mudstones and mudstones, interbedded with red and greyish-green siltstones, mudstone bands, and gypsum laminations. In general, its weathered colors are red and green. It contains fossil ostracods and freshwater fishes, which are deposited in the lacustrine deposits. Its thickness is in range of 270~1000 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

In the type section, the Jidike Fm conformably contacts with the underlying Oligocene Suweiyi Fm.

Upper contact

In the type section, the Jidike Fm conformably underlies the Miocene Kangcun Fm.

Regional extent

The formation is distributed to the region ranging from Kuche to Rouqiang, northwest and south of the Tarim Basin.


GeoJSON

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Fossils

Pisces: Tungtingichthys sp.. Ostrocoda: Cyprinotus (Heterocypris) orientalis, C. (H.) incurvas, C. (H.) formalis, C. (H.) ampulius, C. (H.) detaria, Eucypris longa, E. concinna, E. kaktalensis, E. inftata, E. normalis, E. simplex, Cypria acutus, Darwinula silentiasa, Psuedoeucypris kerkiensis, Hemicyprinotus valvaetunidus, Limnocythere cinctura, Mediocypris schneiderae, Cypridopsis arctica.


Age 

China Lexicon chart schematically shows it as mid-Early Oligocene through Early Miocene.

Age Span: 

    Beginning stage: 
Rupelian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
30.60

    Ending stage: 
Burdigalian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
15.99

Depositional setting

It is interpreted as a river depositional environment.


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