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Song Hien Formation
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Song Hien Fm base reconstruction

Song Hien Fm


Period: 
Triassic

Age Interval: 
Early Triassic, T1, (3)


Province: 
Viet Bac

Type Locality and Naming

Song Hein Basin. The type section is located on the dirt road from Pac Giai to Ma Phuc, on the left side of the Song Hien River, to the west of Cao Bang Town (N = 22°35’; E = 106° 14’).

Synonym: Schistes de Song-hiem (part.): Bourret R. 1922 (Anthracolithique moyen - Triassique moycn). Điệp Sông Hiếh (part.): Vasilevskaia E.D. 1962, (in Dovjikov A.E. et al. 1965.); Vũ Khúc 1989, 1990 (Trias hạ - trung), (in Vũ Khúc et al. 1965, 1986) (Trias trung-thượng); Nguyễn Kinh Quốc (in Vũ Khúc, Bùi Phú Mỹ et al. 1990) (Trịas hạ - trung). Hệ tầng Sông Hiến: Vũ Khúc, Đặng Trần Huyên 1995; Đặng Trần Huyên 1996; Vũ Khúc et al. 2000 (Trias hạ). Điệp Sông Hiến (part.): Phạm Đinh Long 1975 (Anísi); Trịnh Thọ (in Trần Văn Trj et al. 1977 (Trias trung). Các irầm tích Ânisi: Vũ Khúc (in Dương Xuân Hảo et al. 1980). Điệp Bình Gia: Nguyễn Kinh Quốc, Đặng Trần Huyên (in Nguyễn Kinh Quốc et al. 1991).


Lithology and Thickness

Terrigenous with thick intervals of volcanics in lower parts of some sections. Section from Binh Gia Townlet to BanHuan Village (Lang Son Province; 760 m thick): (1). Polymictic conglomerate and gravelstone containing some boulders of limestone, and tuffaceous gritstone shale containing some coaly matter; 100 m thick; containing Induan bivalve Claraia gervilliaeformis. (2) Dacite, rhyolite, rhyolitic tuff with lenses of greenish-grey andesite-basalt and basalt; 100 m thick. (3) Rhyolitic tuffs, tuffaceous sandstone and gritstone, yellowish-grey tuffaceous sandy siltstone; grading upward into rhyodacite, dacite and their tuffs; 250 m thick. (4) Greyish fine-grained sandstone, siltstone and shale; 110 m thick, containing Claraia species.


Lithology Pattern: 
Volcanics


Relationships and Distribution

Lower contact

This formation rests unconformably upon Upper Paleozoic limestone (Bac Son Fm; although uppermost Permian Dong Dang Fm is also in this region), as has been observed in the sections west of Cao Bang Town and in the Binh Gia area.

Upper contact

Unconformably underlies the Anisian-age Lan Pang Fm, as observed only in the Lan Pang area.

Regional extent

The Song Hien Fm is widely distributed and occupies almost all the Song Hien Depression. It extends from the Pho Bang, Yen Minh, Cao Bang areas in the north, southeastward to the Binh Gia, Diem He and That Khe areas of Lang Son Province.


GeoJSON

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Fossils

Fossils are rare in the formation. In its extensive distribution area only some fossil localities have been found in the above-described sections. They can be subdivided into two levels: 1) that with Lytophiceras and Claraia, collected from the lower part of the formation, belonging to the Claraia-Eumorphotis Assemblage, known in Viet Nam as an Induan fauna, 2) that with Olenekian ammonoids Anakashmirites and Dieneroceras, collected from the upper part.


Age 

Dated by the fossils as Early Triassic.

Age Span: 

    Beginning stage: 
Induan

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
251.90

    Ending stage: 
Olenekian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
246.70

Depositional setting


Depositional pattern:  

Additional Information


Compiler:  

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).