Duyantang Fm
Type Locality and Naming
East Guizhou. The Duyantang Fm (uppermost formation unit of the Fanjingshan Gr) was named by the Party of Regional Geological Survey, Guizhou Bureau of Geology in 1974. The type section is in Duyantang, Waxi Township, Jiangkou County, Guizhou Province. Uppermost formation in the Fanjingshan Gr.
Synonym:
Lithology and Thickness
The Duyantang Fm is dominated by light grey to grey-green medium- to thick-bedded blasto-psammitic greywacke, intercalated with blasto-sandstone, siltstone and thin-bedded sericite slate and silty slate. The ripple marks are seen occasionally. The maximum exposed thickness of this formation is recorded as 784 m.
[Figure: The stratigraphic column of the Fanjingshan Gr (the group is about 1000 m thick). a. Pillow lava of the Huixiangping Fm.; b. The boundary between the underlying Fanjingshan Gr and the Furongba Fm (= lower Jialu Fm?) which is the basal formation of the Xiajiang Gr.]
Relationships and Distribution
Lower contact
The formation is in conformable contact with underlying the Waxi Fm of the Fangjingshan Gr
Upper contact
It is unconformably overlain by the Hongzixi Fm of the Banxi Gr, or the Jialu Fm of the Xiajiang Gr
Regional extent
East Guizhou. But it is exposed only in east sector of Fanjing Mt.
GeoJSON
Fossils
Age
Depositional setting
Additional Information