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
Xiayao Formation

Xiayao Fm


Period: 
Permian

Age Interval: 
P3 , Wuchiapingian Stage (early Lopingian Epoch; early Late Permian)


Province: 
Hubei

Type Locality and Naming

The type section is located in the Xiayao area of Huangshi City, Hubei Province.It was named by Wang Shaowei et al., in 1966.


Lithology and Thickness

Limestone. Its lower part represents a suite of light-grey to dark-grey medium-bedded and thick-bedded cherty concretion-bearing limestones. Only a local segment has thin-bedded siliceous rocks, or with the dolomite occurring in its upper part. Variable thickness; with range from about 5 to 200 m.


Lithology Pattern: 
Siliceous limestone


Relationships and Distribution

Lower contact

Conformable contact with the Longtan Fm

Upper contact

Conformable contact with the Dalong Fm

Regional extent

Although its thickness is not so great, yet the formation is stable in its distribution in the Yangtze stratigraphic region. Its thickness is of 10-30 m in the southeastern part of Hubei Province, and is getting smaller in a direction from south to north. In the West Hubei-Southwest Hubei, its thickness is commonly of about 15-58 m, locally (for instance, in the area of Jinjia’ao of Changyang County) being of over 200 m. In the area to the east of the Ziqiu Country of Changyang County to Songzi City the formation has facially changed into siliceous rocks of the Dalong Fm. In the Jingshan-Nanzhang area it is only 4-7 m thick and is thinning out in the area extending from the northwestern part of the Nanzhang County to Baokang County. In the area of south Anhui to south Jiangsu provinces, the formation is commonly regarded as the Top Limestone Member of the Longtan Fm, known locally as the Coal-pressing Limestone, with a thickness of less than 10 m.


GeoJSON

null

Fossils

In the area of south Anhui to south Jiangsu provinces, it yields abundant Brachiopod fossils such as Neophricodothyris waageni, N. asiatica, Squamularia calori, Dictyoclostus margritatus, Spinomaginifera kueichowensis, Tyloplecta yangtzeensis, Edristeges kayseri, Cathaysia chonetoides, Leptodus nobilis, etc.; Fusulinids such as Codonofusiella schubertelloides, C. paradoxical, C. lui, Palaeofusulina parafusiformis, P. nana, P. fluxa, Reichelina simplex, etc.; and Corals such as Waagenophyllum simplex, Tachylasma lopingense, etc.


Age 

Wuchiapingian Stage (early Lopingian Epoch; early Late Permian)

Age Span: 

    Beginning stage: 
Wuchiapingian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
259.55

    Ending stage: 
Wuchiapingian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
254.24

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Shang Qinghua