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Chabaoma Formation

Chabaoma Fm


Period: 
Neogene

Age Interval: 
Miocene, N1, (8d)


Province: 
Qinghai

Type Locality and Naming

The lectostratotype is Buyihu section (N33°28′00″, E90°10′00″), Zhiduo County, Qinghai Province. According to the manuscript, named by Xia Zhu in 1957. Introduced by the Regional Stratigraphic Table Compilation Group of Qinghai Province in 1980.

Synonyms: The Chabaoma Formation is synonymous with the Shipingding Fm and the Chapangmaxun Gr.


Lithology and Thickness

The continental volcanic rocks of the Chabaoma Formation are mainly neutral volcanic lava, such as trachyandesite and andesite. The lower part is composed of grayish-black, grayish-green, reddish-brown, spheroidal and porphyry lava. The upper part is composed of light-gray and grayish-black porous lava. The thickness ranges from 80 m to 1841m.


Lithology Pattern: 
Lava


Relationships and Distribution

Lower contact

The Chabaoma Formation overlies the Tuotuohe Fm or the Bayankelashan Gr, the Jiezha Gr and the Fenghuoshan Gr.

Upper contact

The Chabaoma Formation is overlain by the Quguo Fm and the Qiangtang Fm.

Regional extent

Zhiduo County, Qinghai Province. (Hoh Xil basin Tanggula Mountain)


GeoJSON

null

Fossils

No fossil has been found yet.


Age 

According to the isotopic ages, the ages range from 24.6 Ma to 10 Ma.[For Lexicon graphic purposes with adjacent and overlying/underlying uncertain age spans; put here as only late-Early through early-Late Miocene.]

Age Span: 

    Beginning stage: 
Burdigalian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
20.45

    Ending stage: 
Tortonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
7.25

Depositional setting

Continental volcanic deposits.


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Sukuan Hou, J.Z. Qigao, Q. Li, Q.Q. Shi, B.Y. Sun, S.Q. Wang, F.X. Wu