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Tumenzi Formation

Tumenzi Fm


Period: 
Neogene

Age Interval: 
Miocene, N1, (14a,b)


Province: 
Jilin, Heilongjiang

Type Locality and Naming

The type section is located at north Tumenzi in Chunhua Village, Hunchun County, Jilin Province. It was named by Okada S. and Nisida V. in 1940 and was resurveyed by the Jilin Geological Bureau in 1978. Geographical coordinates of the type section: 43°16′00″N, 131°4′00″E (GPS).

Synonym: Tumentzu Series, Tomonsi Series; It is synonymous with Ma’anshan Fm.


Lithology and Thickness

It is characterized by the sandstones, conglomerates, clays, and diatomite. In the diatomaceous earth, there are one or two layers of basalts, whose thickness varies from several meters to dozens of meters. The thickness of Tumenzi Fm is 420 m.


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

The Tumenzi Fm is in faulted contact with the underlying Hunchun Fm.

Upper contact

The Tumenzi Fm is in in unconformable contact with the overlying Chuandishan Fm.

Regional extent

The Tumenzi Fm is distributed in Hunchun City, east of Jilin Province, and in west Heilongjiang as well.


GeoJSON

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Fossils

Plants: Zelkova, Quercus, and Betula. Sporopollen assemblages: Quercoidites- Ulmipollenites- Liquidambarpollenites. Diatoms are also found in this formation.


Age 

The age of the intercalated basalt layer is 11.3-28.4 my according to isotopic dating.

Age Span: 

    Beginning stage: 
Aquitanian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
23.04

    Ending stage: 
Serravallian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
11.63

Depositional setting

Lacustrine clastic deposits.


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