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Rilagou Formation

Rilagou Fm


Period: 
Triassic

Age Interval: 
Late Early Triassic (TJ74)


Province: 
Sichuan

Type Locality and Naming

Sichuan Diaoduan and Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (1982) collectively referred to the Early Triassic Induan-Olenekian strata in western Sichuan as the Boatigou Fm. In 1991, Sichuan Bureau of Geology and Mineral Resources separated the upper strata of the Botzigou Fm (Bocigou Fm) and named it Rilagou Fm, which was determined to be the Early Triassic Olenekian.

Synonym:


Lithology and Thickness

It is gray with purplish red, grayish green, brown slate, crystalline limestone and a little siltstone. Purplish red or brown is the striking mark of this group, and it is the top and bottom boundary mark of this group.


Lithology Pattern: 
Pelagic marl


Relationships and Distribution

Lower contact

It is conformable with the underlying Bocigou Fm

Upper contact

Pseudo-conformable with the overlying Zagashan Fm

Regional extent

The lithology is stable and the thickness is generally 30 to 100 m. Distributing in Sichuan Luhuo, Songpan, New Jin, Rang Tang area. In the area of Songpan Gold Panning Gou, the formation overlaps over the Permian system.


GeoJSON

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Fossils

It contains conodonts Neospathodus waageni, N. collinsoni, N. timorensis, Neogondolella jubata and Gladigondolella tethydis.


Age 


Age Span: 

    Beginning stage: 
Olenekian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
249.88

    Ending stage: 
Olenekian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
246.70

Depositional setting

It is interpreted as warm, normal marine deposits.


Depositional pattern:  


Additional Information


Compiler:  

Zhang Shunxin, Xiong Feng and Tong Jinnan.