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Tien Hung Formation
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Tien Hung Fm base reconstruction

Tien Hung Fm


Period: 
Neogene

Age Interval: 
Late Miocene; N13, (12, 13)


Province: 
Vietnam Offshore North

Type Locality and Naming

Hanoi Depression and North Song Hong Basin (north Red River Basin). The type section is located borehole GK.4 drilled in the Tien Hung District area (Thai Binh Province) from 250 to 1010 m (N = 20°34’; E =106°18’).

Synonym: Hệ tầng Tiên Hưng: Golovenok V.K., Lê Văn Chân 1966; Golovenok V.K., Kisliakov V.N. 1970; Phan Trung ĐiỀn 2000; Trịnh Dánh (in Vũ Khúc et al. 2000). Diệp Tiên Hung: Trần Đình Nhân, Trịnh Dánh 1975; Sevostianov K.M. 1977; Phạm Hồng Quế 1981; Lê Văn Cự 1987; ĐỖ Bạt, Phan Huy Quynh 1984, 1986, 1993,2000; IDEMITSU 1994. Diệp Đông Hoàng: Lê Vãn Cự 1987. Miocene: TOTAL 1992.


Lithology and Thickness

It is composed of clearly rhythmic sediments with the rhythms beginning with gritstone, sandstone grading upward to siltstone, claystone, coaly shale and many brown coal seams. In these rhythms, the coarse-grained part is usually thicker than the fine-grained part. There are as many as 15-18 rhythms. Sandstone and gritstone are usually feebly cemented or friable, bearing garnet, with poorly sorting and rounded grains. In the lower part of the formation, the beds are usually strongly compressed, and contain interbeds of white-grey calcareous sandstone bearing siderite concretions. The thickness of the formation in this borehole reaches 760 m.

The coal-bearing level decrease is clearly caused by the increasingly seawards marine depositional environment with the marine character. Sandstone is light grey to greenish-grey colored, fine- to coarse-grained, thick-bedded to massive structure, poor to medium sorting, with carbonate-clay cement, bearing fauna and brown coal debris. Silty claystone is greenish-grey to light grey, locally brownish-grey, black-grey colored (boreholes GK.104, 102-HD) bearing fossils and coal debris, locally, glauconite and pyrite (boreholes GK.100, 103-TH). The thickness of the formation changes from 760 to 3000 m.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Unconformably upon the Phu Cu Fm.

Upper contact

Unconformably under the Vinh Bao Fm.

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[106.18,19.88],[106.71,18.87],[107.56,17.71],[108.68,16.81],[108.81,16.95],[108.72,17.99],[107.53,19.54],[107.44,20.25],[107.17,20.47],[106.62,20.34],[106.18,19.88]]]]}}

Fossils

Dacrydium, Ilex, Quercus, Castanea, Pinus, Liquidambar, Tsuga, Florschuetzia trilobata, FI. levlpoli, Leguminosae, Euphorbiaceae, Carya, Alnus and the spores Cyathea, Magnastriatites howardi, Acrostichum, Cleichenia, Stenochlaena of the Assemblage Dacrydium-Ilex-Quercus - FI. trilobata.


Age 

Late Miocene.

Age Span: 

    Beginning stage: 
Tortonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
11.63

    Ending stage: 
Messinian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
5.34

Depositional setting

Deltaic plain environment with swamps (the coal layers).


Depositional pattern:  

Additional Information


Compiler:  

Discussion notes from Prof. Tran Nghi (2019); Tran Van Tri and Vu Khuc (Editors; Geology and Earth Resources of Viet Nam, General Dept. of Geology and Minerals of Viet Nam; completed in Dec., 2011), with additional details from Tong-Dzuy Thanh and Vu Khuc (Editors; Stratigraphic Units of Viet Nam, 2nd edition; 2011; English edited by A. Boucot).