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Tiejianggou Formation

Tiejianggou Fm


Period: 
Neogene

Age Interval: 
Early-Late Miocene, N


Province: 
Gansu

Type Locality and Naming

The type section is Tiejianggou section, located at the Dangchengwan Township, Subei Mongol Autonomous County. Geographical coordinates: 39°29′20.93″N, 94°41′14.79″E (GPS). It was named by Wang et al., in 2003.

[Figure: Outcrops of the Xishuigou section. A, strong folding in the Tiejianggou Formation. B, the bottom fault contact with the underlying unnamed strata.]


Lithology and Thickness

The lithology upwardly thickens. Lower part is characterized by light brown massive mudstone with gray-green sandstone, fine conglomerate and thin-bedded siltstones; Middle part comprises light reddish brown sandstone, siltstone, mudstone and gray-brown sandstone, coarse sandstone, glutenite interbedded; Upper part dominated by gray-red, gray-brown massive conglomerate, breccia mixed with reddish brown sandstone, siltstone and mudstone. The thickness is larger than 2600 m.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

It is in fault contacts with the underlying Paoniuquan Fm.

Upper contact

It is in fault contacts with the overlying unnamed Late Miocene to Pliocene strata.

Regional extent

It is distributed in Subei Mongol Autonomous County and Aksai Kazakh Autonomous County along the north foothill of the Dangjinshan Mountains.


GeoJSON

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Fossils

Rodentia: Sayimys obliquidens, Heterosminthus sp. Litodonomys xishuiensis; Perissodactyla: Phyllotillon sp., Artiodactyla: Turcocerus sp., Amphiomschus sp.; Proboscidea: Platybelodon dangheensis; Carnivora: Schultzogale sp.,


Age 

Burdigalian through mid-Tortonian (T. Deng et al., 2019, China Integrated Stratigraphy and TimeScale; Neogene chapter).

Age Span: 

    Beginning stage: 
Burdigalian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
20.45

    Ending stage: 
Tortonian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
9.44

Depositional setting

Predominantly fluvial-lacustrine deposits, partially pluvial/alluvial fans.


Depositional pattern:  


Additional Information


Compiler:  

Tao Deng, Sukuan Hou, J.Z. Qigao, Q. Li, Q.Q. Shi, B.Y. Sun, S.Q. Wang, F.X. Wu