Song Ma Fm
Type Locality and Naming
Holostratotype: the Hoi Xuan - Lang Bai Section, lying along Road No.217, Quan Hoa District, Thanli Hoa Province (N= 20°22', E= 105°06'). Tran Huu Dan (in Pham Kim Ngan et al.) 1998, 2000
Synonym: -H4 tang Song Ma: Ph^m Kim Ng^n in Tran Van Trj et aL 1973, 1975, 1977 (£2)» ^ Ducfng XuSn Hao el al 1980 (£2); Ph?un Kim Ng^a et ai 1986, L991, 1994, 1995, .1996, 2000 (£2); Luong H6ng Hu(?c in Le Himg, T6ng Duy Thanh et al 1987 (£2); Nguyln Dinh K<^p et al 1993 (£J; Nguyln VSn Hoanh et al 1994 (£2); Luofng H6ng Hir^c
et aL 1996 (£2); Tr^n Hiiu Dk\ in Ph^m Kim Ngan et al 1998 (£ 2); Ph^m Dinh Tru6ng et at. 1999 {£2); Nguyin Van Tru^t et al L999 (£2); T<Sng Duy Thanh in Vu Khuc et al 2000; Dinh C6ng Hung et al 2001 (£2)- -D'4p Song Md: Vu Khuc, Bui Phu My et al. 1990 (£}; Phan C\r Tien et al. 1989 (£); Ph^im Xuan Anh et al, 1989 (£2); D§ Van Chi et al. 1992 (e2). -tdng BdThu&c (partly.]>lgayh\TriVziet al. 1963 {£3). -ff^ tang Bin Khe (part.): Nguyin Tri VM et al 1963 (£3). -H4 tang Dong San (part.); Jamoida A.I. in Dovjikov A.E. et al. 1965 (£r〇). -H4 tdngBen Khi (part.): Dovjikov A. E. et ai) 1965 (£3-0). -Middle Cambrian: Ph^m Kim Ngan 1972, 1975, 1976; Phan Cyr Ti^n et al. 1997, 1978; Bui Phu My 1978; Tr4n Dang Tuylt e, “/• 1978; Trin Nghla d 1980; D^ng TrAn Qudn 以 “/_ 1980; Luong H6ng Hugrc 1980.
-H$ tdng Diin Lu (pari.): Ph$m Van Quang et ai 1973 (£2); Tong Duy Thanh et ai 1995 (E2)*
-Di^p BoXinh (part.): Phan Scm etal 1974, 1978 (&2-0). Di^p Lan^Khuong (part.): Dinh Minh Mpng et al. 1976, 1978 (£2)- tdng Ha Giang: Ph^un Kim Ngan 1982 (£2); Luomg H6ng Hu<?c 1986, 1987. (£2)
Lithology and Thickness
Characteristic sequence along the Lo River from Hoi Xuan to Bai Villate (Quan Hoa District) is 600-700 m of mainly schist with interbeds of limestone. Luong River section is 330 m: (1) Sericite-shale and cherty shale; 180 m. (2) Thin-bedded recrystallized limestone with some interbeds of sericite shale; 40 m. (3) Banded quartzite interbedded with carbonate-bearing schist and light-grey limestone; 60 m; with trilobites of Middle Cambrian. (4) Dark-grey recrystallized limestone interbedded with sericite-quartz schist; 50 m.
Relationships and Distribution
Lower contact
Unconformably upon the Nam Co Fm (PR3 - Cm1 nc),
Upper contact
Conformable below the carbonate sediments of the Ham Rong Gr (Cm2 - Oi)
Regional extent
Two narrow and discontinuous bands in NW-SE direction (Same extent as the overlying Ham Rong Gr). First band extends from the Pha Din Pass (Lai Chau Province) to Ban Mo through Na Vien (Son La Province) through Laos to Quan Hoa, Ham Rong Bridge and Ba Trieu Temple (Thanh Hoa Province). Second band is from Co Ma, Chieng Dong (Son La Province) through Laos to Luong and Lo Rivers (Thanh Hoa) areas.
GeoJSON
Fossils
Middle Cambrian trilobites characterize the adjoining beds between Middle and Upper Cambrian, such as: Cyclolorenzella sp.? Damesellidae and Agnostidae, found in sericite schist, on Road No.217 about 2 km S-SE of Ta Lang Village.
Age
Depositional setting
Additional Information