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Taiyangling Formation

Taiyangling Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, (TJ10a, TJ10b).


Province: 
Jilin

Type Locality and Naming

It was named by the Coalfield Searching and Prospecting Party of Jilin Province as the “Taiyangling Coal Series” in 1971, and was first cited publicly by the Compiler

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of Jilin Province, and was renamed as the Taiyangling Formation in 1978. The naming section is located in the Banshidingzi area extending to the Taiyang Ridge of Shuangyang County, Jilin Province, with its reference section being situated in the vicinity of the Jiguan Mts about 2 km south of the Wujia Coal Mine.

Synonym: (太阳岭组)


Lithology and Thickness

Lower part is composed of medium- and fine-grained sandstones intercalated with gritstone, thin-bedded conglomerate, siltstone, mudstone and coal beds. Upper part is composed of conglomerate, intercalated with sandstone and thin-bedded acid volcaniclastics; with a thickness of about 1144 m.


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

Its basal part is in a disconformable contact with the underlying Banshidingzi Fm. It Nanloushan region of Jilin, the schematic stratigraphic column indicates it can be unconformable on the late Triassic Lujiatun Fm.

Upper contact

Regionally, the next younger unit is indicated as Xiajiajie Fm

Regional extent

It is distributed largely in the areas of Taiyang Ridge, Liushuhezi and Bamianshi of the Shuangyang Basin. In addition, the conglomerates intercalated with volcanic clastic deposits exposed in the area of Sihetun Village of Huadian County may also belong to the formation.


GeoJSON

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Fossils

It yields plant fossils as represented by the middle-stage assemblage of the Coniopteris-phoenicopsis flora, component members of which are Equisetum multidentatus, E. cf. laterale, Neocalamites sp., Todites williamsoni, Coniopteris hymenophylloides, Cladophlebis argutula, C. asiatica, Nilssonia sp., Ginkgo sp., Phoenicopsis sp., Czekanowskia rigida, C. setacea and Taeniopteris sp.


Age 

Schematic strat column suggests Aalenian age.

Age Span: 

    Beginning stage: 
Aalenian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
174.70

    Ending stage: 
Aalenian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
170.90

Depositional setting

The formation represents fluvial and swamp-facies deposits in the intermontane basins.


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of Jilin Province, and was renamed as the Taiyangling Formation in 1978. The naming section is located in the Banshidingzi area extending to the Taiyang Ridge of Shuangyang County, Jilin Province, with its reference section being situated in the vicinity of the Jiguan Mts about 2 km south of the Wujia Coal Mine.

Synonym: (太阳岭组)

Lithology and Thickness:

Lower part is composed of medium- and fine-grained sandstones intercalated with gritstone, thin-bedded conglomerate, siltstone, mudstone and coal beds. Upper part is composed of conglomerate, intercalated with sandstone and thin-bedded acid volcaniclastics; with a thickness of about 1144 m.

Lithology-pattern: Coarse-grained sandstone

Relationships and Distribution:

Lower contact:

Its basal part is in a disconformable contact with the underlying Banshidingzi Fm. It Nanloushan region of Jilin, the schematic stratigraphic column indicates it can be unconformable on the late Triassic Lujiatun Fm.

Upper contact:

Regionally, the next younger unit is indicated as Xiajiajie Fm

Regional extent:

It is distributed largely in the areas of Taiyang Ridge, Liushuhezi and Bamianshi of the Shuangyang Basin. In addition, the conglomerates intercalated with volcanic clastic deposits exposed in the area of Sihetun Village of Huadian County may also belong to the formation.

GeoJSON:

Fossils:

It yields plant fossils as represented by the middle-stage assemblage of the Coniopteris-phoenicopsis flora, component members of which are Equisetum multidentatus, E. cf. laterale, Neocalamites sp., Todites williamsoni, Coniopteris hymenophylloides, Cladophlebis argutula, C. asiatica, Nilssonia sp., Ginkgo sp., Phoenicopsis sp., Czekanowskia rigida, C. setacea and Taeniopteris sp.

Age:

Schematic strat column suggests Aalenian age.

Age span:

Beginning stage: Aalenian

Fraction up in beginning stage: 0.0

Beginning date (Ma):

Ending stage: Aalenian

Fraction up in ending stage: 1.0

Ending date (Ma):

Depositional setting:

The formation represents fluvial and swamp-facies deposits in the intermontane basins.

Depositional-pattern:

Additional Information

Compiler

Jingeng Sha (coordinator)