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Ergulazi Formation

Ergulazi Fm


Period: 
Triassic

Age Interval: 
Early-middle Late Triassic, (TJ67)


Province: 
Jilin

Type Locality and Naming

Liu Maoqiang and Mi Jiarong were named in 1981. The named profile is located in Yihe District, Naozhigou Township, north of Linjiang Town, Jilin Province.

Synonym: In 1996, the National Stratigraphic Multiple Division and Comparative Study of the Jilin Province Littostratigraphic Compilation Group classified the Ergu Lizi Formation into the Changbaishan Fm, and the age is T3-J1. Study on multiple stratigraphic division and correlation of the abandoned Naozhigou Fm and Ergulizi Fm in Jilin, the two strata are collectively called Changbai Fm (Cao, 1994).


Lithology and Thickness

Mainly neutral lava, consisting of lava breccia—neutral and basic lava—neutral lava forming intermittent volcanic eruption cycles. The thickness is 1880~2175 m.


Lithology Pattern: 
Lava


Relationships and Distribution

Lower contact

It is in unconformity contact with the underlying strata

Upper contact

It is in conformity contact with the overlying Naozhigou Fm

Regional extent

Distributed on the line of Hualizi Mountain-Caiyuanzi West Mountain in Naozhigou Township, Hunjiang City, Jilin Province, it is distributed in a near east-west direction.


GeoJSON

null

Fossils

No fossils have been seen.


Age 

Shown on schematic stratigraphic section as spanning Carnian-Norian.

Age Span: 

    Beginning stage: 
Carnian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
237.00

    Ending stage: 
Norian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
205.74

Depositional setting

This group is a set of andesite, andesitic volcanic clastic facies.


Depositional pattern:  


Additional Information


Compiler:  

Cao Hongsheng, Ji Kaixuan and Tong Jinnan.