Mai Hung Fm
Type Locality and Naming
Mae Hong Son basin (NW Thailand), near Myanmar, north of Mae Ping Fault. Named after Mai Hung village, Mueang Mae Hong Son district; type section is at a limestone cave, about 1.5 km along the track SSE of Mai Hung village (grid reference 878067 on map sheet 4547-II). Middle formation in the Huai Pong Gr.
Synonym: หมวดหินไม้ฮงุ
[Figure: The three sedimentary basins in which the marine Jurassic occurs, and their relationships to the main faults which might subsequently have displaced them (MYF, Mae Yuan Fault; MPF, Mae Ping Fault; TPF, Three Pagodas Fault; KMF, Khlong Marui Fault). The main outcrop areas of non-marine Jurassic rocks are also shown. In some areas, particularly on Peninsular Thailand, the Jurassic succession contains both marine and non-marine facies (redrawn from Meesook 1994; Charusiri et al. 2002, by Meesook A. & Saengsrichan W., 2011, Page 152).]
Lithology and Thickness
Sandy limestone. Well-bedded sandy limestone with oncolites in the lower part (Unit C); a fossiliferous calcareous siltstone (unit D); massive grey limestones in the middle part (Unit D); and sandy limestone in the upper part (Unit E). Thickness: at the type section and 70 m at Huai Ta Pu Kho in Mae Sot District, Tak Province.
Relationships and Distribution
Upper contact
Grading into sandstone of the overlying Kong Mu Fm.
Regional extent
Mae Hong Son basin (northern part of Mae Hong Son – Kanchanaburi Basin); Northern Region: Mae Hong Son and Tak provinces
GeoJSON
Fossils
An Aalenian age is given for the formation on the basis of the foraminifer Timidonella sarta Bassoullet et al.
Age
Depositional setting
Shallow marine, neritic zone
Additional Information