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Shezi Formation

Shezi Fm


Period: 
Triassic

Age Interval: 
Late Late Triassic (TJ70, TJ101)


Province: 
Yunnan

Type Locality and Naming

The type section is located at Shezi Village near the Burma Road 4 km north of Feng Country and Langping Town, Yunnan. It was named by Chen Guangyuan, Zhang Kai and Xu Hongyou in 1943. It is equivalent to the uppermost coal-bearing strata of Yipinglang Coal Measure, which lies between Fengjiahe Fm of Lower Jurassic and Ganhaizi Fm of Upper Triassic, and represents the middle and late Late Triassic. Lu Zhaoqia and Wang Hengsheng (1936) established the Yipinglang Coal Series, which was dated as the Late Triassic. In 1943, Chen Guangyuan et al. further divided Yipinglang Coal Measures into Pujiacun Fm, Ganhaizi Fm and Shezi Fm in order, and regarded as the Late Triassic Norian.

Synonym: Shezhi Fm (spelling).


Lithology and Thickness

Lower part is mainly composed of grayish-black, yellowish-green and yellowish-brown carbonaceous shale intercalated with coal seams. Upper part is mainly composed of grayish-green, yellowish-green, purple, purplish-red sandstone and fine sandstone intercalated with mudstone.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

The Shezi Fm is conformable in contact to the sandstone and siltstone of underlying Ganhaizi Fm with a bed of grayish-yellow, gray block medium sandstone.

Upper contact

This formation is conformable in contact to the purplish-red mudstone and grayish-green, grayish-purple quartz sandstone of overlying Fengjiahe Fm or Xialvfeng Fm

Regional extent

The formation is distributed widely along the Lvzhi river and Yilangping. The thickness varies largely ranging from 320 to 671 m. This formation is equivalent to the Shezi Fm in Lvfeng, Baoding Fm in Yongren, and Baitutian Fm in Xiangyun.


GeoJSON

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Fossils

Bivalves: Modiolus aff. frugi;Plants: Dictyophyllum nathorsti, Clathropteris meniscioides, Ptilozamites chinensis, Pterophyllum ptilum, Anthrophyopsis crassinervis; Ostracoda: Darwinula medialis; Conchostracans: Euestheria minuta.


Age 

In 1956, the 560 Team of Southwest Geological Bureau thought it belonged to the Late Triassic. Si Xingjian and Zhou Zhiyan believed that it belonged to the Late Triassic Norian to Rhaetian. According to the book Regional Geology of Yunnan Province (1990), Ganhaizi Fm and Shezi Fm belong to the Late Triassic Norian to Rhaetian.

Age Span: 

    Beginning stage: 
Norian

    Fraction up in beginning stage: 
0.9

    Beginning date (Ma): 
207.90

    Ending stage: 
Rhaetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
201.36

Depositional setting

It is interpreted as coal-bearing deposits in marine and continental interchange.


Depositional pattern:  


Additional Information


Compiler:  

Zhou Huiqin, Wu Yuyang and Tong Jinnan.