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Mihei Formation

Mihei Fm


Period: 
Silurian

Age Interval: 
the Rhuddanian to Aeronian of Llandovery (S1), (29, 30)


Province: 
Sichuan

Type Locality and Naming

The name Mihei Fm was given by the First Party of Regional Geological Survey, Sichuan Bureau of Geology in 1965 and published by the Compiling Group of Regional Stratigraphical Scale of Sichuan Province in 1978. The type section is located at Miheigou, north of Xiqiu Township in Muli Tibetan Autonomous County, Sichuan Province.

Synonym: (米黑组)


Lithology and Thickness

The Mihei Fm, 208 m thick, consists of dark gray-grayish black siliceous slate intercalated with gray metamorphosed quartzose sandstone, minor phyllite and crystalline limestone.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

The formation disconformably contacts onto the underlying Lower Ordovician.

Upper contact

The formation disconformably contacts the overlying Lower Carboniferous. Regionally, the next younger unit is the Gezhadi Fm of late-Early Silurian.

Regional extent

It is 190 m thick at Shuilehe in Muli and is intercalated with basic volcanic rock at Dingyangpengzai of Muli totaling 830 m in thickness.


GeoJSON

null

Fossils

It yields graptolites Glyptograptus cf. persculptus, Petalolithus minor, Monograptus cf. sedgwickii, etc.


Age 

Early Silurian, but Glyptograptus cf. persculptus [=Normalograptus persculptus ?] suggests extends into Hirnantian; as is shown on schematic stratigraphic section in Silurian chapter.

Age Span: 

    Beginning stage: 
Hirnantian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
444.14

    Ending stage: 
Aeronian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
438.59

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng