Chentangwu Fm
Type Locality and Naming
North-central Zhejiang. The Chentangwu Fm was named by the Gong Rixiang and Yan Tiezeng in 2009. The typical section is situated in Chengtangwu village in Pujiang County, Zhejiang Province. Coordinate: 27°32.00´ N; 109°58.00´E.
[Figure: The holotype section and column of strata of the Chentangwu Fm in the Zhejiang Province. A-C-Sampling in tuff beds of the Chengtangwu Formation; B-Pillow lava developed in the Mengshan Formation; D-Sampling in the Mengshan Formation in the Chengtangwu reservoir in Pujiang County, Zhejiang Province.]
Synonym: (陈堂坞组)
Lithology and Thickness
The Chentangwu Fm is composed of feldspathic quartz debris siltstone, mudstone with tuff and pebble coarse sandstone, sandy gravel, mud-siliceous rocks with a thickness is over 624 m.
Relationships and Distribution
Lower contact
The Chentangwu Fm is conformably overlying the Mengshan Fm [Not in current Lexicon. " The authors consider that the Mengshan Formation,which is below the Chentangwu Formation,is correlated with the lava pillow and spilite of the Shaoqiwa Formation in Lushan area." [Gao Linzhi and Ding Xiaozhong, 2013, Geol. Bull. China, 32: 988-995]. Regionally, the Chencai Gr (Xu'an Fm) would be the next older unit.
Upper contact
Its top part is a fault contact to Cretaceous sandstone.
Regional extent
The Chentangwu Fm is restrictedly distributed in Chentangwu, Pujiang County, Zhejiang Province.
GeoJSON
Fossils
Age
Depositional setting
Additional Information