Dangchong Fm
Type Locality and Naming
The type section is located at Dangchong of Baohetang area, Shaodong County, Hunan Province. It was named by Tian Qizhun and Xu Reilin in 1936.
Lithology and Thickness
Limestone and Shale. It is divisible into two parts. Lower part above a basal black shale is composed of grey calcareous slate and clayey limestone, intercalated with carbonaceous shale, with a thickness of 14 m. Upper part consists of grey and dark-grey thin- and medium-bedded limestones, intercalated with shale, siliceous rocks and skeletal limestone, with a thickness of 82 m. The lithology of the formation is fairly stable, and its thickness reaches as great as 120 m.
Relationships and Distribution
Lower contact
Conformable contact with the underlying Qixia Fm
Upper contact
Conformable contact with the overlying Leping Fm
Regional extent
Distributed to the south of an alignment of Ma’anshan, Qiaotou and Douli Mt. areas, Xinhua County, Hunan Province, as well as at Huangfengqiao and Guanghuang of Youxian County and Shanshan Mt. of Hengshan County, Hunan Province, with its thickness getting greater from south to north, and with the limestone interbeds increasing in amount, thus resulting in a facies change of it into the limestone of the Maokou Fm.
GeoJSON
Fossils
The Dangchong Fm in the Qujiang and Renhua areas is found to yield Radiolaria fossils (Song Tianrui et al., 1977).
Age
Depositional setting
It is interpreted as fairly deep-water basin deposits.
Additional Information