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Tarlang Formation

Tarlang Fm


Period: 
Permian

Age Interval: 
P (7), late-Early and Middle Permian


Province: 
Xinjiang

Type Locality and Naming

The type section is located at the Taoshuyuan about 40 km to the northwest of the Daheyan Railway Station, Tulufan, Xinjiang. It was named by Xinjiang Petroleum Administration in 1973, and was cited officially by the Compiling Group for the Regional Stratigraphic Chart of the Xinjiang Uygur Autonomous Region in 1981.


Lithology and Thickness

Marl and Clastics. Lower part is composed of unequal interbeds of purple-grey and grey-green thin-bedded marl, conglomerate and sandstone Upper part is composed of dark-purple and yellow-green sandy siltstones, intercalated with conglomerate. Thickness is 411 m.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

Conformable contact with the dark-grey conglomerate of the underlying Daheyan Fm

Upper contact

Conformable contact with the overlying Quanzijie Fm conglomerate

Regional extent

Distributed in the Yila Lake and the Korjie area in the western part of Xinjiang, as well as in the area to the west of the Danan Lake in the southeastern part of Keya Region of North Xinjiang.


GeoJSON

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Fossils

Its lower part yields fish fossil represented by Turfania taoshuyuanensis; Ostracoda represented by Tomiella-Microdonta assemblage; bivalves represented by Anthraconauta-Mrasiella-Microdonta; plant fossils (phytolites) such as Callipteris altaica, Comia dentate, C. yichunensis and spore-pollen fossils.


Age 

Previously assigned (Permian Lexicon version, 2017) as mid-Middle Permian, but if "conformable on Daheyan Fm", then implied to begin in mid-Sakmarian (lower Early Permian) according to Shuzhong Shen et al. (2019, Permian integrated stratigraphy and timescale of China)!

Age Span: 

    Beginning stage: 
Sakmarian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
292.02

    Ending stage: 
Capitanian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
259.55

Depositional setting

It is interpreted as a lake-river-facies


Depositional pattern:  


Additional Information


Compiler:  

Hou Jingpeng