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Zhangkezhai Formation

Zhangkezhai Fm


Period: 
Jurassic

Age Interval: 
Lower Jurassic, J1 (TJ51)


Province: 
Yunnan

Type Locality and Naming

It was named by the No. 16 Geological Party under the Geological Bureau of Yunnan Province in 1966. The naming locality is situated at the Zhangkezhai Village 18 km west of the Pu’er County town, Yunnan Province, with the section in the Nanbangpo area of Dehua region, Pu’er County serving as its reference section.

Synonym: (张科寨组)


Lithology and Thickness

Lower part is composed mainly of purple and grey-violet mudstones, siltstones and fine-grained sandstones, intercalated with yellow and grey-green mudstones and siltstones, with its basal part consisting of lime-conglomerates and sandy conglomerates. Middle part consists of brown-red and violet massive mudstones and silty mudstones, intercalated with yellow-green and grey mudstones, siltstones and fine-grained sandstones. Upper part is thick alternating layers of grey-yellow, violet-grey and grey fine- to medium-grained sandstones in association with purple and violet mudstones and siltstones, with the sandstones containing pebbles locally. Its total thickness is of 1096 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

It is in a disconformable contact with the underlying Dapingzhang Fm (column TJ51).

Upper contact

Coeval with sandy claystone of Yangjiang Fm in same region. In Pu'er graphic column, next younger unit had been indicated as early-Middle Jurassic clayey sandstone of Huekalzuo Fm.

Regional extent

The formation is distributed in the Jinggu, Pu’er, Simao and Mengla county regions, with its lithology being consistent from region to region, but with increase of the basal sandy conglomerate in thickness (600 m) in the Xiaohewan area of Jinggu County. And there are greater variations in the total thickness of the formation, being in a range from tens of meters to 1600 meters.


GeoJSON

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Fossils

Its lower part yields clam shrimps such as Palaeolimnadia diannanensis, P. longyinensis and P. longmenshanensis; bivalves such as Pseudocardinia sibireconchiformis and P. khadjakalanensis.


Age 

Indicated as "Lower Jurassic", therefore pending details, shown here as Hettangian-Toarcian

Age Span: 

    Beginning stage: 
Hettangian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
201.36

    Ending stage: 
Toarcian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
174.70

Depositional setting


Depositional pattern:  


Additional Information

Bureau of Geology and Mineral Resources of Yunnan Province (1996) abandoned the Zhangkezhai Formation for its ambiguous definition and chaotic citations.


Compiler:  

Jingeng Sha (coordinator)