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Maoshan Formation

Maoshan Fm


Period: 
Silurian

Age Interval: 
the Lower Telychian of Silurian (S1), (62, 63)


Province: 
Jiangsu, Anhui

Type Locality and Naming

Li Yurau et al (1935) proposed the name Maoshan Sandstone with the type section located at Dinggong, Maoshan, about 60 km south of the Jurong County seat, Jiangsu Province. The lateral equivalent/ similar to Maoshan, Juken Fm was proposed by the Anhui Party of Regional Geological Survey (1982) with the type section located at Juken, 3 km north of Xinming, northeast of Xianyuanzhen Town, Huangshan City in southern Anhui Province.

Synonym: (茅山组)


Lithology and Thickness

The formation, 115 m in total thickness, is subdivided into three parts. The Lower part consists of grayish white fine-grained quartzose sandstone intercalated with thin-bedded purplish red siltstone (with cross-bedding). The Middle part is purplish red medium-to-fine-grained quartzose sandstone intercalated with siltstone and sandy shale. The Upper part gray, grayish yellow and grayish white medium- to fine-grained quartzose sandstone.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

It is continuous deposited from the underlying Fentou Fm

Upper contact

It is pseudo-conformably overlain by the basal conglomerate of the Wutong Fm of the Upper Devonian.

Regional extent

It is widely exposed in south Jiangsu Province in thickness ranging from 40~200 m. According to the sedimentary criteria (e.g., the huge cross-beddings), the formation probably represents different parts of the underwater delta deposits and might belong to marine-terrestrial alternating deposits (Chen Xu et al, 1988). The formation is only 20-30 m thick and consists of purplish red thick-bedded sandstone, intercalated with gray sandstone at the base in the adjacent area of Nanjing City. The Juken Fm is basically similar to the Maoshan Fm in lithology, biofacies and horizons. This lateral equivalent Juken Fm is composed of purplish red, yellowish green and grayish white quartzose sandstone, fine-grained sandstone and argillaceous siltstone.


GeoJSON

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Fossils

The Maoshan Fm bears rare fossils, only Sinogaleaspis, and bivalve, algal Leiopsophosphaera, Trachysphaeridium, Lophosphaeridium, etc.

The only fossil finds are the low differentiated littoral fauna such as brachiopod Lingula, gastropod, bivalve and fish in the lateral equivalent Juken Fm


Age 


Age Span: 

    Beginning stage: 
Telychian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
435.76

    Ending stage: 
Telychian

    Fraction up in the ending stage: 
0.8

    Ending date (Ma):  
434.06

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng