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
Wayaobao Formation

Wayaobao Fm


Period: 
Triassic

Age Interval: 
Late Triassic, (TJ53, TJ54)


Province: 
Shaanxi

Type Locality and Naming

It was named in 1934 by Pan Zhongxiang. The named section is located in Zichang County, Shaanxi Province (Wayaopu); the reference section is located in Qishuihe, Tongchuan, Shaanxi Province. Uppermost formation of the Yanchang Gr.

Synonym: Wayaopu Fm. The name “Wayaopuo Coal-bearing” refers to the strata integrated above the Yanchang bed. Most of the strata are grey sandstone, shale and black shale, the lower part contains several layers of coal, coal line, age is defined as early Jurassic. Wang Shangwen (1950) discovered an erosional surface in the Wayaopu coal-bearing, and thus classified the strata above the erosional surface as Jurassic. The Northwest Mesozoic and Cenozoic stratigraphic conference (1976) renamed the Wayaopu Formation and dated to the Late Triassic. The Institute of Geology of the Chinese Academy of Geological Sciences (1980) classified it as the top of the Yanchang Fm, corresponding to the fifth member of the original Yanchang Fm. Regional Stratigraphic Table of Shaanxi Province (1983) and Regional geological records of Shaanxi Province (1989), The study of multiple division and correlation of strata in Shaanxi Province (1994) is classified as the Wayaopu Formation of Yanchang Group. [Tong et al., 2019, and other English-language entries in the Triassic portion of the Lexicon use a spelling of Wayaoboa, so this is adopted here.]


Lithology and Thickness

Characterized with the interbeds of yellow green, gray black and gray yellow mudstone with sandstones and siltstones, and interbedded with multi-layer coal seams or black shales, with thickness of 224 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

This formation is in conformable contact with the underlying Yongping Fm

Upper contact

It is in disconformable contact with the overlying Jurassic Fuxian Fm

Regional extent

Mainly distributed in Yijun, Shenmu, Zichang, Yongping, Fu County, Tongchuan and other places, due to different degrees of erosion, resulting in a greater change in thickness.


GeoJSON

null

Fossils

Rich in animal and plant fossils. Plants: Danaeopsis fecunda, Bernoullia zeilleri, Cladophlebis gigantea, Cl. raciborskii, Todites shensiensis, Nilsssonia pterophyllloides, Thinnfeldia nordenskioldi, etc.; Ostracoda: Darwinula, Tungchuania, etc.; Bivalves: Shaanxiconcha.


Age 

Tong et al. (2019; Triassic integrative stratigraphy and timescale of China; Science China: Earth Sciences, 82: 189-222) indicate that it is early through middle Rhaetian.

Age Span: 

    Beginning stage: 
Rhaetian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
205.74

    Ending stage: 
Rhaetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
201.36

Depositional setting

The Wayaopu Fm (Wayaobao Fm) is swamp-lacustrine facies.


Depositional pattern:  


Additional Information

In 1959, Gan Kewen and others renamed the "Yanchang Series", and divided 5 lithological members and included the lower strata of the "Wayaobao Coal System" built by Pan Zhongxiang. In 1980, the Institute of Geology of the Chinese Academy of Geological Sciences named the first and second members of the Yanchang Series as the Tongchuan Fm, and the age was Middle Triassic; The third, fourth, and fifth members are named "Yanchang Fm", and their ages are the Late Triassic. Regional Geology of Shaanxi Province combined Tongchuan Fm, Hujiacun Fm, Yongping Fm and Wayaopu Fm as Yanchang Gr, in which, Tongchuan Formation equal to the first and the second member of Yanchang Gr; Hujiacun Fm, Yongping Fm and Wayaopu Fm (Wayoaboa Fm) equal to the third, fourth and the fifth member correspondingly.


Compiler:  

Cao Hongsheng, Yu Yingyue and Tong Jinnan.