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Ganheba Formation

Ganheba Fm


Period: 
Mesoproterozoic

Age Interval: 
Xishanian (Ectasian) Xs (32)


Province: 
Sichuan

Type Locality and Naming

Central Sichuan (Ya'an). The Ganheba Fm was named by Zhang Honggang in 1983, The type section is in the region of Maiyanglin-Ganheba, Dayi County and Huangshuihe, Changshiba, Lushan County, Sichuan Province. It is the lowermost formation in the Huangshuihe Gr.

Synonym: (干河坝组)


Lithology and Thickness

In the type section, the Ganheba Fm is dominated by grey-green, grey-purple metamorphosed basalt, andesite, intercalated with spilite, volcanic breccia, tuff and graphite schist, schist. The rocks in the lower part are mostly metamorphosed to actinolite schist and grey-purple tuffite. The thickness varies from 300 m to over 2000 m.


Lithology Pattern: 
Lava


Relationships and Distribution

Lower contact

Bottom is not seen. It does not directly contact with Kangding Complex Gr.

Upper contact

The top is in conformable contact with overlying Huangtongjianzi Fm (lower Huangshuihe Gr).

Regional extent

Central Sichuan (Ya'an). The formation is distributed mainly in Dayi, Lushan, Baoxing and Pengxian counties, Sichuan Province.


GeoJSON

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Fossils


Age 

The schematic stratigraphic column places it as spanning Xishanian (Ectasian).

Age Span: 

    Beginning stage: 
Ectasian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
1,400.00

    Ending stage: 
Ectasian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
1,200.00

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.