Minh Hoa Fm
Type Locality and Naming
Holostratotype - The unique section of the formation occurs on the northern side of Minh Hoa Island (also called Hon Nghe Island), Kien Giang Province, in the Gulf of Thailand (N = 10°02'; E = 104°34’). The formation bears the name of this island..
Synonym: - Hệ tầng Minh Hoà: Nguyễn Xu.n Bao et ai. 1991, 2000 (Anisi); Nguyễu Ngọc Hoa el ./.1995; Vũ Kh.c (in Vũ Kh.c eí ai. 2000 (Anisi). - Calcaire ?Permien: Fontaine H., 1968. - Hệ tầng Hòn Nghệ (part.): B.i Ph. Mỹ, Vũ Kh.c 1980 (T2 ); Vũ Kh.c, B.i Ph. Mỹ et aí. 1990 (T2 ). - Dá vôi Hòn Nghệ: Vũ Kh.c (irt Tống Duy Thanh el ai. 1995 - Anisi).
Lithology and Thickness
Limestone: The section includes only light-grey, thick-bedded to massive limestone, approximately 200 m thick.
Relationships and Distribution
Lower contact
The lower boundary has not been observed on the island. Regionally, the next older formation is the Permian Dat Do Fm.
Upper contact
Tectonic contact with the Jurassic Ta Pa Fm lying on the northern side of the island through a NW-SE trending fault; there the fault left a thin zone of tectonic breccias.
Regional extent
Gulf of Thailand
GeoJSON
Fossils
Foraminifera and hexacorals (not studied). Foraminifera were determined by Doan Nhat Truong, including Endotelỉa controversa, E. sp. (ex gr. E, bithynica), E. badouxi, Diplotremina astrofimbriata, D. sp., Duostroma sp., Pilaminella falsofriedu, and Malayspira fontainei of Anisian-Ladinian age.
Age
Depositional setting
Additional Information