Sa Pa Gr
Type Locality and Naming
Upper formation of the Cha Pa Gr. The type section is located in 25 km southwest of Lao Cai Town (N = 22 0 23', E = 103 ° 52'). It was named after the Da Dinh mountain/village by Nguyen Van Hoanh et al., 2000.
Synonym: Điệp Dá Đinh (Upper Proterozoic): Kalmykov A.F.; Trần Văn Trị 1965. Série de Sa Pa: Jacob C. 1921 (Algonkien). Série de Coc Xan (part.): Fromaget J. 1937. (Algonkien supérieur). Hệ tầng Sa Pa (Upper Proterozoic): Bùi Phú Mỹ et al. 1971. Trần Văn Trị et al. 1977. Hệ tầng Chiêm Hoá (part.): Dovjikov A.E. et al. 1965 (Proterozoic)
Lithology and Thickness
Characteristic section at Da Dinh Mt is 600 m thick: (1). Fine to medium-grained, medium-bedded tremolite-bearing sugary-texture marble, grading upwards into fine- to coarse-grained dolomitic marble and white, medium-bedded to massive dolomite; 250 m thick. (2). White, medium-grained, thick-bedded to massive dolomitic marble interbedded with banded marble containing tremolite, muscovite and scapolite; 350 m thick.
Relationships and Distribution
Lower contact
Conformably upon the Cha Pa Fm.
Upper contact
Unconformably beneath conglomerate of the Lower Cambrian Cam Duong Fm.
Regional extent
Bands and small massifs of limestone mountains scattered from Lao Cai Province to Yen Bai Province.
Correlative with the Dongying Fm limestone in Yunnan of Sinian age.
GeoJSON
Fossils
No fossils.
Age
Depositional setting
Additional Information