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Nieniexiongla Formation

Nieniexiongla Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, (TJ46)


Province: 
Xizang (Tibet)

Type Locality and Naming

It was named by Mu Enzhi as the Nieniexiongla Group in 1973. The naming section is located in the vicinity of the Nieniexiongla area at the No. 10-11 Maintenance Squad of the Dingri-Nyalam Highway.

Synonym: (聂聂雄拉组)


Lithology and Thickness

Lower part of the formation consists of alternating layers of grey medium-bedded limestones and argillaceous limestones, intercalated with sandy shales, grey-black medium-, and thin-bedded limestones, grey-white medium-, and coarse-grained quartz-sandstones, yellow-green sandy shales, siltstones and poststones (=fine-grained sandstone). Middle part consists of dark-grey thick-bedded limestones, grey-white quartz-sandstones, intercalated with limestones. Upper part consists of alternating layers of dark-grey medium-, and thin-bedded limestones, sandy limestones and quartz-sandstones, intercalated with grey-black and yellow-green shales. It is 1639 m in thickness.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

Its basal part is in a fault contact with the lower Cretaceous Series. Regionally, the next older unit is the Pupuga Fm of earliest Jurassic.

Upper contact

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

Regional extent

The formation is distributed mainly in the areas of Nieniexiongle, Lalongla Pass, Dingri and Jilong, with a consistent lithology and with a thickness of 600-1500 m.


GeoJSON

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Fossils

It yields in the Nieniexiongla region abundant ammonites, bivalves, Brachiopoda and Gastropod fossils. Among the ammonites fossils there are found Witchellia tibetica, W. sayni, Dorsetensia haydeni, D. xizangensis, D. cf. edauardiana, Macrocephalites sp., M. compressus, M. cosmopolitum, Indocephalites spaeroidalis and I. Diadematus; of bivalves there are found Trigonia (T.) brevicostata, T. (T.) cf. brevicostata, Camptonectes les, C. cf. laminatus, Variamussium pumilum, Ostrea (Liostrea) acuminata and Cucullaea cf. egertoniana.


Age 

Schematic strat column in previous "red Chinese Lexicon" had implied that the Nieniexiongla Fm spanned the Middle Jurassic.

Age Span: 

    Beginning stage: 
Aalenian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
174.70

    Ending stage: 
Callovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
161.53

Depositional setting

The formation represents typical littoral and shallow-sea deposits.


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)