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Bulukqi Formation

Bulukqi Fm


Period: 
Ordovician

Age Interval: 
Mid-Late Ordovician, (2)


Province: 
Xinjiang

Type Locality and Naming

The type section is at Bulukqi (86°34′00″E, 46°46′30″N), Hobokesar County, Northern Xinjiang. The Bulukqi Formation was named at Bulukqi on the southwest slope of the Sharburti Hill in Hoboksar County, northern Xinjiang, by the United Stratigraphic Group of Xinjiang Team of Regional Geological Survey and Institute of Geology and Mineral Resources of Chinese Academy of Geological Sciences in 1973, and was published by Hou Hongfei et al. (1979).

Synonym: (布鲁克其组)


Lithology and Thickness

In the type area, the Bulukqi Formation is represented by an incomplete sequence of yellowish brown, gray, gray green volcaniclastic rock intercalated with limestone. This formation recorded thickness more than 710 m.


Lithology Pattern: 
Volcanic ash


Relationships and Distribution

Lower contact

It is exposed with covered lower boundary in the type section.

Upper contact

It is exposed with covered upper boundary in the type section. Regionally, the next younger unit is the Bulongguor Fm of Katian.

Regional extent

The stratigraphic unit is exposed only in Sharburti Hill.


GeoJSON

null

Fossils

The limestone intercalation yields trilobites Remopleuroides bulukeqiensis and Illaenus; brachiopods Cyclospira koboksariensis and Paramboni; gastropod Maclurites.


Age 

Mid-Late Ordovician. The dating of this formation is difficult, and Xiao Bing (1990) suggested a roughly Mid to Late Ordovician age for it.

Age Span: 

    Beginning stage: 
Darriwilian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
463.80

    Ending stage: 
Katian

    Fraction up in the ending stage: 
0.4

    Ending date (Ma):  
449.73

Depositional setting

It represents shallow sea deposit dominated by submarine volcanic eruption.


Depositional pattern:  


Additional Information


Compiler:  

Jianpo Wang and Xiaofeng Wang