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Hongtiegou Formation

Hongtiegou Fm


Period: 
Cambrian

Age Interval: 
possibly middle and late Meishucunian (late early-Cambrian) (40)


Province: 
Qinghai

Type Locality and Naming

Type section of Hongtiegou Formation is the Quanjishan section, located at Heitupo in Hongtiegou Village, near Quanjishan Mountain, Da Qaidam, Haixi Prefecture, Qinghai Province (95°51’E, 37°25’N). The section lies about 60 km southeast of Da Qaidam Town, and was remeasured by Wang Yunshan and Chen Jiliang from Qinghai Institute of Geological Survey in 1983. It is the moddle portion of the same type section shared by the underlying Heitupo Formation and overlying Zhoujieshan Formation, each embraces the Bed 1‒3 and Bed 7‒10 respectively, while the Hongtiegou Formation embraces the Bed 4‒6. In the type section, the formation is 17.50 m thick.

Synonym: (红铁沟组)


Lithology and Thickness

The Hongtiegou Formation is a glacial conglomerate sequence. It includes the middle three beds of the Quanjishan type section (Bed 4 to 6), from bottom up: 4, yellowish green and grey glacial gompholite (5.00 m thick) [NOTE: "gompholite" is a German term from the Alpine molasse basin, and seems to be coarse fluvial deposits]; 5, purple red glacial gompholite with interbeds of yellow calcareous dolomite (thickness of single bed is 2‒6 cm) in the lower part (11.70 m); 6, light greyish green glacial gompholite with obscure lamination (0.80 m).


Lithology Pattern: 
Glacial till


Relationships and Distribution

Lower contact

The Hongtiegou Fm rests disconformably on the underlying Heitupo Fm, but occasionally in conformable contact with the latter formation. The lower boundary of the Hongtiegou Fm is defined by the plane of disconformity

Upper contact

Iis overlain conformably by the thick-bedded dolomite of Zhoujieshan Formation.

Regional extent

The Hongtiegou Formation is exposed in the Qaidam Area of the Qaidam -Qilian-Alexa Region, restricted mainly in the Quanjishan area, Haixi Prefecture, Qinghai Province, and it outcrops also at Shihuigou, which lies about 20 km east of the Quanjishan Mountain. At Shihuigou, the formation is 108 m thick.


GeoJSON

null

Fossils

The formation yields no fossil.


Age 

Based on its stratigraphic position, the formation is possibly middle and late Meishucunian in age. (late early-Cambrian)

Age Span: 

    Beginning stage: 
Fortunian

    Fraction up in beginning stage: 
0.85

    Beginning date (Ma): 
530.47

    Ending stage: 
Cambrian Stage 2

    Fraction up in the ending stage: 
0.45

    Ending date (Ma):  
525.40

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Peng Shanchi