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Miyadani Formation

Miyadani Fm


Period: 
Permian

Age Interval: 
early-middle Middle Permian (Asselian), (15a)


Province: 
Kurosegawa Belt- Shikoku

Type Locality and Naming

Kurosegawa Belt-central Shikoku

Synonym:


Lithology and Thickness

It mainly consists of sandstone, mudstone and alternating beds of sandstone and mudstone, in association with conglomerate and rare acidic tuff.

[Figure 1: Stratigraphy of the Paleozoic of the Kurosegawa Belt in the central part of Shikoku, Southwest Japan (after M. Ehiro et al., 2016)]


Lithology Pattern: 


Relationships and Distribution

Lower contact

Regionally, the schematic strat column indicates the next older unit as Older Ino Metamorphic Complex Fm

Upper contact

Regionally, the schematic strat column indicates the next younger unit as Ichinose Fm

Regional extent

Kurosegawa Belt-central Shikoku. Coeval with Miyanaro Fm


GeoJSON

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Fossils


Age 

Shown as early-middle Middle Permian, hence placed Base of Asselian

Age Span: 

    Beginning stage: 
Asselian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
298.89

    Ending stage: 
Kungurian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
274.37

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Moreno, T., WALLIS, S., Kojima, T. & Gibbons, W. (Eds) 2016. The Geology of Japan. Geological Society. London. 1-24.