Waxi Fm
Type Locality and Naming
East Guizhou. The Waxi Fm was named by Wang Yangeng et al. in 1974. The type section is in Waxi Village, at east sector of Fanjing Mountain, Guizhou Province. Upper formation in the Fanjingshan Gr.
Synonym: (洼溪组)
Lithology and Thickness
The Waxi Fm is of rhythmic layering of greyish, grey-green blasto-sandstone, blasto-siltstone, blasto-tuff, slate and silty slate. Lower part of the formation consists of sandstone, calcareous sandstone and tuff. In the sandstone are developed the oblique bedding and ripple marks. Upper part consists of greyish, grey-green slate and sandy slate. It is recorded 1100 - 1238 m thick.
[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
It conformably contacts with overlying Duyantang Fm
Upper contact
It conformably contacts underlying Tongchang Fm
Regional extent
East Guizhou. It is only developed in Fanjing Mountain, Guizhou Province.
GeoJSON
Fossils
Age
Depositional setting
Rhythmic layering
Additional Information