Xiangkuang Fm
Type Locality and Naming
Northeast peninsula of Shandong. The Xiangkuang Fm was named by the Jiaodong (E. Shandong) Geological Survey of Changchun College of Geology in 1960. It was quoted by the Committee of Stratigraphy of China in 1962. The naming section is located in Xiangkuang Douya, Qixia County, Shandong Province.
Synonym: (香夼组)
Lithology and Thickness
The Xiangkuang Fm consists of a suite of pelitic carbonate. Lower part is mainly gray, blue gray, yellow gray, gray green marl with gray thin-bedded limestone and yellowish gray thin-bedded pelitic limestone with minor calcareous slate. Upper part consists of gray, yellowish gray and dark gray medium- to thick-bedded limestone, dolomitic limestone. In the top part, thick-bedded limestone includes minor black siliceous masses. It is about 1020 m in thick.
Relationships and Distribution
Lower contact
In the bottom, brown gray thin-bedded marl rest conformably on the underlying yellow green slate at top of the Mashan Fm.
Upper contact
The blue gray dolomitic crystalline limestone at the top of the formation shows intrusive contact with granophyric textured granite. In many places, the top part is covered by Quaternary or Cretaceous strata.
Regional extent
Northeast peninsula of Shandong. The formation is distributed locally, which are mainly developed in the Xiangkuang Pb-Zn mine, cement factory and Douya, Qixia County, Shandong Province.
GeoJSON
Fossils
Microplants: Trachysphaeridium sp., Lophominuscula sp., Paleamorpha punctulatea etc; Stromatolites are found in some places.
Age
Depositional setting
Additional Information