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Kezilenur Formation

Kezilenur Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, J2 (TJ14a).


Province: 
Xinjiang

Type Locality and Naming

It was named by Yao Guofan, Tao Ruiming in 1957, and was first cited publicly by the Compiler

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of the Xinjiang Uygur Autonomous Region. The naming section is located at the Kezilenur gully of the Kuche County, Xinjiang (Yao Guofan, Tao Ruiming, 1957, A report on the comprehensive studies on the petroleum geology of the Kuche depression, unpublished). Uppermost formation in Kelasu Gr.

Synonym: (克孜勒努尔组), Kyzylnur Fm (spelling).


Lithology and Thickness

Composed of an alternating layer of grey-green siltstone and black carbonaceous shale in association with grey-white quartz-sandstone, intercalated with coal beds, and with a thickness of 400-800 m.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

It is in a conformable contact with the underlying Yangxia Fm.

Upper contact

Regionally schematic strat column shows this formation as uppermost unit in that Kelasu Gr; and overlain by the Sanjianfang Fm.

Regional extent

The particular formation is distributed in the areas of Kuche, Baicheng and Toksun Counties. There it is characterized by a consistent lithology, but by a greatly changeable thickness as proved by its thickness being of 843.30 m in the Kezilenur gully, and by a thickness of only 486 m in the area of Kapushaliang. In the area of Kelasu the rocks are getting coarser, with an increase in the amount of conglomerate.


GeoJSON

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Fossils

It yields in the Kezilenur gully such plant fossils as Equisetites sp., Coniopteris hymenophylloides, C. tatungensis, Cladophlebis sp., Phoenicopsis angustifolia, Podozamites lanceolatus, Pityophyllum cf. lindstroemi, and Ginkgo cf. digitata. In the Kapushaliang section it yields bivalve fossils as represented by Pseudocardinia asiatica, P. elongata, P. lanceolata, P. ovalis, P. jeniseica, P. tuvensis, Ferganoconcha tomiensis and Sibireconcha anodontoides.


Age 

Schematic stratigraphic column suggests Aalenian (and Bajocian, based on re-assigned age for the overlying Sanjianfang Fm).

Age Span: 

    Beginning stage: 
Aalenian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
174.70

    Ending stage: 
Bajocian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
168.17

Depositional setting

The particular formation belongs to lacustrine deposits.


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of the Xinjiang Uygur Autonomous Region. The naming section is located at the Kezilenur gully of the Kuche County, Xinjiang (Yao Guofan, Tao Ruiming, 1957, A report on the comprehensive studies on the petroleum geology of the Kuche depression, unpublished). Uppermost formation in Kelasu Gr.

Synonym: (克孜勒努尔组), Kyzylnur Fm (spelling).

Lithology and Thickness:

Composed of an alternating layer of grey-green siltstone and black carbonaceous shale in association with grey-white quartz-sandstone, intercalated with coal beds, and with a thickness of 400-800 m.

Lithology-pattern: Siltstone

Relationships and Distribution:

Lower contact:

It is in a conformable contact with the underlying Yangxia Fm.

Upper contact:

Regionally schematic strat column shows this formation as uppermost unit in that Kelasu Gr; and overlain by the Sanjianfang Fm.

Regional extent:

The particular formation is distributed in the areas of Kuche, Baicheng and Toksun Counties. There it is characterized by a consistent lithology, but by a greatly changeable thickness as proved by its thickness being of 843.30 m in the Kezilenur gully, and by a thickness of only 486 m in the area of Kapushaliang. In the area of Kelasu the rocks are getting coarser, with an increase in the amount of conglomerate.

GeoJSON:

Fossils:

It yields in the Kezilenur gully such plant fossils as Equisetites sp., Coniopteris hymenophylloides, C. tatungensis, Cladophlebis sp., Phoenicopsis angustifolia, Podozamites lanceolatus, Pityophyllum cf. lindstroemi, and Ginkgo cf. digitata. In the Kapushaliang section it yields bivalve fossils as represented by Pseudocardinia asiatica, P. elongata, P. lanceolata, P. ovalis, P. jeniseica, P. tuvensis, Ferganoconcha tomiensis and Sibireconcha anodontoides.

Age:

Schematic stratigraphic column suggests Aalenian (and Bajocian, based on re-assigned age for the overlying Sanjianfang Fm).

Age span:

Beginning stage: Aalenian

Fraction up in beginning stage: 0.0

Beginning date (Ma):

Ending stage: Bajocian

Fraction up in ending stage: 1.0

Ending date (Ma):

Depositional setting:

The particular formation belongs to lacustrine deposits.

Depositional-pattern:

Additional Information

Compiler

Jingeng Sha (coordinator)