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Mesoproterozoic

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Bayinxibie Gr

Bayinxibie Gr


Period: 
Mesoproterozoic

Age Interval: 
Jixianian (Calymmian) Jx (5)


Province: 
Inner Mongolia

Type Locality and Naming

Southwestern-most Inner Mongolia. The Bayinxibie Gr was named by Li Pu in 1954. The type locality is in Bayinxibie Mountain in northwest part of Alxa Zuoqi, Inner Mongolia.

Synonym: (巴音西别群)


Lithology and Thickness

It is informally subdivided into lower and upper lithostratigraphic formations with a conformable contact between them. The lower formation is represented by east Bayinxibie section in Alxa Zuoqi, and the upper formation is represented by Zhulazhaga-Maodao section in Alxa Zuoqi and the. Lower formation, 1160 m thick, consists of marl, slate and thin-bedded quartzite, with the upper part intercalated with several intermediate-basic volcanic rock beds. Upper formation, 700 m thick, is composed of blue-grey thick-bedded dolomite, intercalated with minor yellow-grey muddy and silty slate and muddy limestone, while. The group is relatively stable both in lithological facies and thickness. The Bayinxibie Gr is over 1800 m thick.


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

The base of the lower formation is in conformable contact with the Takelinobo Fm of Nuorgong Gr, Changcheng System. However there may be a fault repetition or other structure problem in Bayinxibie Gr section in Bayinxibe region, but this awaits proof.

Upper contact

Schematic stratigraphic column indicates it is disconformably overlain by a Wulanhaxia Gr (not in Lexicon) of Qingbaikouan age; but Alxa column (17) for Neoproterozoic has a Haishenghala Fm of early Qingbaikouan (which might be the lower unit in that Group?)

Regional extent

Southwestern-most Inner Mongolia. The Bayinxibie Gr concentrically spreads at Bayinixibe Mt., Haisheng-Hala, Hala-Wula and Zhulazhaga-Maodao Mt. in northwest part of Alxa Zuoqi, Inner Mongolia.


GeoJSON

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Fossils

The upper formation yields abundant stromatolites, such as Colonnella bayanxibiensis, Tielingella cf. tielingensis, Anabaria f., Conophyton cylindricum, C. favosum, Jacutophyton alaxaensis, Baicalia alaxaensis, Jurusania f., Inzeria f., Tungussia f., and Kussiella f..


Age 

There are no radioisotopic dates available to constrain its geological age. Shown on the schematic stratigraphic column as spanning the Jixianian (Calymmian).

Age Span: 

    Beginning stage: 
Calymmian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
1,600.00

    Ending stage: 
Calymmian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
1,400.00

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Extracts from The Mesoproterozoic Erathem (chapter in Stratigraphic Lexicon of China, draft of 2022) by Gao Linzhi, Ding Xiaozhong, Zhang Chuanheng, Zhang Heng.