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Pac Ma Formation

Pac Ma Fm


Period: 
Triassic

Age Interval: 
Late Carnian, T3, (8, 9)


Province: 
West Bac Bo

Type Locality and Naming

The type section is located on the left side o f the Song Da River, near Pac Ma Village, Quynh Nhai District, Lai Chau Province (N= 21°56’; E= 103°50’).

Synonym: Hệ tầng Pác Ma: Vũ Khúc (in Vũ Khúc et al.) 2000 ịCarni); Vũ Khúc et al 2002. - Calcaire rouge de Pa-m a: Mansuy H. 1912 (Calovi)\ Saurín E. 1956 {Nori hạ). - Đá vôi đó Pác M a: Vũ Khúc 1967 (Carnì-Nori), 1984 (Carni), (in Tống Duy Thanh et al. 1995 - Carni). - Hệ tầng Suối Bàng (part.): Dovjikov A.E. et al.) 1965. - Tầng đá vói ám liêu màu đỏ: Phan Cự Tiến et al. ] 977 (Carni-Norí). - Bậc Carni (part.): Vũ Khúc, Trịnh Thọ (in Trần Văn Tri et al -) 1977, (in Dương Xuân Hào et al.) 1980. - Diệp Nậm Mu (part.): VQ Khúc, Bùi Phú Mỹ et al.) 1990.


Lithology and Thickness

Reef limestone, marl and siltstone; Characteristic section on the Da River bank is Reddish, thick-bedded coral reef limestone (80 m) grading upwards into greenish-grey, thin-bedded marl and siltstone (20 m), containing poorly preserved bivalves. In the north of Yen Chau Townlet, the Pac Ma Fm reaches up to 220 m in thickness.


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

Conformably lies upon clayey shale of the Nam Mu Fm containing the Camian bivalve Zittelihalobia cf. rugosa.

Upper contact

Not clear. Regionally, next younger regional unit is the Nam Po Fm of early Jurassic.

Regional extent

Pac Ma area near the Quyuh Nhai Coal Mine (Lai Chau Province) and as a narrow band extending from the Tat Heo Village (previoius Pho Village) eastwards to the Muong Lum Coal Mine (Son La Province). [NOTE: Lexicon user map-interface is slightly misleading here, because it would be ca. mid-way between columns 7 and 9; on level with 8).


GeoJSON

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Fossils

Corals Thecosmilia sp. and Isastrea sp, and Brachiopods Rhaelina bamaensis, R. cf. complanata, Aulacothyropsis bisinuata, snd Holcorhynchia vietnamica, the Bivalve Halobia pacmaensis at the base.


Age 

Upper Carnian.

Age Span: 

    Beginning stage: 
Carnian

    Fraction up in beginning stage: 
0.6

    Beginning date (Ma): 
231.18

    Ending stage: 
Carnian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
227.30

Depositional setting

Marks the end of the sea regression at the end of the Carnian in the Song Da-Tu Le Basin.


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).