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Kuzigongsu Formation

Kuzigongsu Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, J2 (TJ16, TJ17).


Province: 
Xinjiang

Type Locality and Naming

It was named by the Compiler

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of the Xinjiang Uygur Autonomous Region in 1981. The naming section is located at Xiaoheiziwei Village in the lower reaches of the Kuzigongsu River, Wucha County, Xinjiang.

Synonym: (库孜贡苏组)


Lithology and Thickness

Composed of thick-bedded and massive red conglomerates, intercalated with sandstone and sandy mudstone, with pebbles getting coarser in an ascending order. In many places of the Xiaoheziwei section there occur quartz-sandstone and muddy quartz-sandstone with cross-beddings.


Lithology Pattern: 
Aus conglomerate


Relationships and Distribution

Lower contact

The formation is in a conformable contact with the underlying Ta’erga Fm

Upper contact

It is in an unconformable contact with the overlying Kezilesu Gr (Sanjianfang Fm)

Regional extent

The particular formation is distributed mainly in the area of Kuzigongsu River-Xiaoheiziwei-Tuoyun northeast of Wucha County. A more Compiler

Jingeng Sha (coordinator) exposure of the particular formation is found along the Kuzigongsu River in the vicinity of Wucha County. Southerly it is found to occur in the areas of Tarmu, Shalayi, and Yigeziya to the west of Yingjisha. Besides, it is also found to occur in the area of Buya-Pixi of Hetian County, as well as in the area of Taxidaban of Arkin Mts. The thickness of the formation is changeable from place to place, being of only 160 m in Tuoyun County, while in the area of Arkin Mts its thickness is of 500-1100 m.


GeoJSON

null

Fossils

No fossils have been found there.


Age 

Its geological age was determined on the basis of its stratigraphic position relative to both its overlying and underlying stratigraphic horizons. Schematic strat column suggests Bathonian-Callovian age (implying major hiatus at top).

Age Span: 

    Beginning stage: 
Bathonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
168.17

    Ending stage: 
Callovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
161.53

Depositional setting

The formation represents fluvial facies.


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of the Xinjiang Uygur Autonomous Region in 1981. The naming section is located at Xiaoheiziwei Village in the lower reaches of the Kuzigongsu River, Wucha County, Xinjiang.

Synonym: (库孜贡苏组)

Lithology and Thickness:

Composed of thick-bedded and massive red conglomerates, intercalated with sandstone and sandy mudstone, with pebbles getting coarser in an ascending order. In many places of the Xiaoheziwei section there occur quartz-sandstone and muddy quartz-sandstone with cross-beddings.

Lithology-pattern: Aus conglomerate

Relationships and Distribution:

Lower contact:

The formation is in a conformable contact with the underlying Ta’erga Fm

Upper contact:

It is in an unconformable contact with the overlying Kezilesu Gr (Sanjianfang Fm)

Regional extent:

The particular formation is distributed mainly in the area of Kuzigongsu River-Xiaoheiziwei-Tuoyun northeast of Wucha County. A more Compiler

Jingeng Sha (coordinator) exposure of the particular formation is found along the Kuzigongsu River in the vicinity of Wucha County. Southerly it is found to occur in the areas of Tarmu, Shalayi, and Yigeziya to the west of Yingjisha. Besides, it is also found to occur in the area of Buya-Pixi of Hetian County, as well as in the area of Taxidaban of Arkin Mts. The thickness of the formation is changeable from place to place, being of only 160 m in Tuoyun County, while in the area of Arkin Mts its thickness is of 500-1100 m.

GeoJSON:

Fossils:

No fossils have been found there.

Age:

Its geological age was determined on the basis of its stratigraphic position relative to both its overlying and underlying stratigraphic horizons. Schematic strat column suggests Bathonian-Callovian age (implying major hiatus at top).

Age span:

Beginning stage: Bathonian

Fraction up in beginning stage: 0.0

Beginning date (Ma):

Ending stage: Callovian

Fraction up in ending stage: 1.0

Ending date (Ma):

Depositional setting:

The formation represents fluvial facies.

Depositional-pattern:

Additional Information

Compiler

Jingeng Sha (coordinator)