Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Donghe Gr

Donghe Gr


Period: 
Cretaceous

Age Interval: 
Early Cretaceous, (14b) K1dG


Province: 
Shaanxi, Gansu

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.


Lithology Pattern: 
Coarse-grained sandstone


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

null

Fossils

See component formations


Age 


Age Span: 

    Beginning stage: 
Berriasian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
143.10

    Ending stage: 
Hauterivian

    Fraction up in the ending stage: 
0.4

    Ending date (Ma):  
130.16

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wan Xiaoqiao