Donghe Gr
Type Locality and Naming
Zhao Yazeng and Huang Jiqing erected the Donghe conglomerate in 1931. The type locality is in Shuangshipu of Fengxian, Shaanxi Province.
The Donghe conglomerate was assigned to Jurassic or Early Cretaceous (the authors considered that the Donghe conglomerate is exactly the same as the Qianfoyan bed). In 1943 Yang Zhongjian and Bian Meinian renamed the Donghe conglomerate as the Donghe series. In 1944 Ye Lianjun and Guan Shichong called the coal measures in the Huaya area of Chengxian of Gansu the “Jishan coal measures” and the strata under them were still called the Donghe conglomerate, collectively called the Donghe series”. In 1968 the Shaanxi Regional Geological Survey Team called the strata mentioned above as the Donghe Group, which can be divided into three subgroups, the lower, the middle and the upper. In the report entitled “The Preliminary Study on the Characteristics and Age of the Coal-bearing Sediments of the Donghe Group of the Huicheng Basin”, Qi Hua (1974) divided the Donghe Group in the ascending order into the Tianjiaba Fm, Zhoujiawan Fm and Huaya Fm formations. Of them, the “Huaya Formation” has the same implication as does the “Jishan coal measures”, which have all been assigned to Early Cretaceous. In 1994 the Gansu Lithostratigraphic Sorting Group discarded the “Huaya Formation”, renamed it the Jishan Formation and placed it on the Donghe Group. Now the Donghe Group is divided in ascending order into the Tianjiaba Fm and the Zhoujiawan Fm.
Lithology and Thickness
The Donghe Formation is represented by purple red and gray green conglomerate with sandstone and mudstone.
Relationships and Distribution
Lower contact
Its base marked by poorly-sorted conglomerate lies unconformably on the phyllite of the Upper Silurian Bailongjiang Gr. However, next older unit on regional scale is the Permian Shiguan Fm.
Upper contact
Its conformable top marked by purple red and yellow green siltstone and silty mudstone is distinguished from the Jishan Fm marked by gray black conglomerate.
Regional extent
It occurs in the Qinling area at the juncture of Shaanxi and Gansu.
GeoJSON
Fossils
See component formations
Age
Depositional setting
Additional Information