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Songdagou Formation

Songdagou Fm


Period: 
Cambrian

Age Interval: 
Jiangshanian and early Niuchehean (late Cambrian) (44)


Province: 
Sichuan

Type Locality and Naming

The type section of the Songdagou Formation is Jianding-Longyong section. The section is located near Songdagou in Zongza District, Batang County, Sichuan Province (99°22’30”E, 29°19’30”N). It lies about 6.1 km east of the seat of Zongza Township and was measured by the Sichuan Third Regional Survey Team in 1974. In the type section, the formation is over 2017.12 m thick, but there may have overlap of strata due to fault cutting. The Songdagou Formation was named by the No. 2 Brigade of Sichuan Third Regional Geological Survey Team (1977). The name is derived from Songdagou in Zongza District, Batang County, Ganzi Tibetan Autonomous Prefecture, western Sichuan Province.

Synonym: (颂达沟组)


Lithology and Thickness

The Songdagou Formation is mainly a metamorphic clastic sequence, composed of greyish green and greyish yellow phyllitic slate, interbedded with find-crystalline limestone and silty slate in the lower part (ca. 700 m thick); greyish green siltstone, interbedded with quartzose sericitc-phyllite, yellow sericitic slate interbedded with sandy slate, and grayish green phyllite, alternated with silty sericitic slate in the middle part (ca. 470 m); greyish yellow, greyish green slate, silty slate, thin-bedded to massive siltstone, grayish green and grayish yellow phyllite, intercalated with medium- to coarse- crystalline limestone or limestone lenses in the upper part (ca. 850 m).


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

The Songdagou Fm rests conformably on the carbonate Eding Fm

Upper contact

It is conformably overlain by the Upper Cambrian-Lower Ordovician Banggui Fm or disconformably by the Middle-Upper Ordovician Wuluochipu Fm.

Regional extent

The Songdagou Formation, as well as the underlying Eding Fm, is exposed in the Qangtang-Simao Region, scattered in a north-south direction within the Batang County.


GeoJSON

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Fossils

The interval of 30 m thick in the top of the formation yields late Furongian trilobites Calvinella sp. and Haniwa sp. and brachiopod Finkelnburgia. In addition to Calvinella and Haniwa, the formation also yield trilobites Mictosaukia in other locality in Zongza area.


Age 

The fossil from the top of the formation indicates a latest Jiangshanian through early half Niuchehean age. Since a thick sequence lies below, the formation is possibly Jiangshanian through early half of Niuchehean age.

Age Span: 

    Beginning stage: 
Jiangshanian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
494.20

    Ending stage: 
Cambrian Stage 10

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
488.93

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Peng Shanchi