Huangtian Fm
Type Locality and Naming
Southernmost Sichuan. The Huangtian Fm was named by Yang Xianhe in 1976. The type section is in Xinjietian-Xinping, Yanbian County, Sichuan Province. Lowermost formation-level unit of Yanbian Gr.
Synonym: (荒田组)
Lithology and Thickness
In the typical section, the Huangtian Fm is composed of grey green metamorphosed volcanic rock and minor metamorphosed sedimentary rock. Lower part consists of metamorphosed pillow basalt, basaltic volcanic breccia, sandwiched with sericite slate, green schist of 758 m thick. Middle part, 690 m thick, is of siliceous slate, slate, phyllite and chert, occasionally sandwiched with metamorphosed basalt. Upper part, 1490 m thick, consists of metamorphosed basalt (trachybasalt and anamesite [anamesite is a term for basaltic rocks which are between basalt and dolerite in texture]), metamorphosed basalt breccia, with minor siliceous slate. The top consists of metamorphosed andesite, metamorphosed andesitic tuffaceous breccia. It is <3000 thick.
Relationships and Distribution
Lower contact
Bottom is not seen.
Upper contact
The formation is conformably or disconformably overlain by the Yumen Fm.
Regional extent
Southernmost Sichuan. It is distributed mainly around Yumen, Yanbian County, Sichuan Province.
GeoJSON
Fossils
Age
Depositional setting
Additional Information