Gucheng Fm
Type Locality and Naming
The Gucheng Fm was named by Ma Guogan et al. in 1984. The typical section is located at Gucheng 5.5 km southeast of Gaojiayan, Changyang County, Hubei Province.
Synonym: (古城组) , Its synonyms or coeval formations include the Pingqian Formation in Shennongjia area of west Hubei, the Tiesi'ao Fm in northeast Guizhou and the Dongshanfeng Fm in west Hunan.
Lithology and Thickness
The Gucheng Fm is composed of greenish gray tilly sandy gravel or pelodite, in which the gravels are disorderly and unsystematically arranged, have a great disparity in grain size, and display complex compositions including sandstone, siltstone, granite, vein-rock, marl and other carbonates. The gravels are poorly rounded, generally with striations. The thickness varies from several meters to about ten meters. It has with an unstable thickness from 3 to 17 m.
Relationships and Distribution
Lower contact
The Gucheng Fm rests disconformably on the underlying Liantuo Fm
Upper contact
Regional extent
The Gucheng tillite is mainly distributed in Hunan, Hubei, Sichuan and Guizhou provinces..
GeoJSON
Fossils
microplants: Trachysphaeridium laminaritum, Stictosphaeridium implexum, Quadratimorpha jugata, Favososphaeridium sp. Anguloplanina rhombica, Laminarites antiquissimus, etc.
Age
Depositional setting
Additional Information