Van Lang Fm
Type Locality and Naming
An Chau and Song Hien basins. Named after Van Lang Coal Mine (Thai Nguyen Province); described by Ta Hoang Tinh and Pham Dinh Long (1966).
Synonym:
Lithology and Thickness
Coal-bearing. Van Lang Coal Mine has 170-230 m of: (1) Basal conglomerate, 20-80 m. (2) Black-grey calcareous sandstone and siltstone, thin-bedded clayey limestone; and in the upper part, interbeds of coaly shale and coal seams (20 cm to 9 m, with thickest being 16 m!); 100 m; with bivalves and leaf imprints. (3) Light-grey, medium- to coarse-grained quartz sandstone, conglomerate and gritstone, grading upward into dark-grey siltstone and shale, 55 m.
Relationships and Distribution
Lower contact
Unconformable on the Mau Son Fm of Carnian.
Upper contact
Unconformably underlies the Ha Coi Fm of Early-Middle Jurassic.
Regional extent
Change in facies and coal-bearing levels from the west eastward: The section n the west, such as in the Van Lang, Lang Cam, Phan Me, Ba Son and Quan Trieu (Thai Nguyen Province) and Khao Que and Luc Ra (Tuyen Quang Province) areas has the lower part of marine facies and the upper part containing fat coal of industrial significance. But in the west, such as in the Chu and Deo Chinh areas (Bac Giang Province), the section belongs mainly to the brackish to marshy facies and has not coal-bearing significance. Besides, this formation still occurs in the Song Hien Basin in small areas formed along faults.
GeoJSON
Fossils
Bivalves include Unionites species.
Age
Depositional setting
Additional Information