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Hutian Formation

Hutian Fm


Period: 
Carboniferous

Age Interval: 
C12 (29), middle Late Carboniferous


Province: 
Shanxi, Hebei, Beijing, Liaoning, Shandong, Jiangsu, Henan

Type Locality and Naming

The type section is located in the Hutian mining district of the Zibo Coalfield, Shandong. It was named by Guan Sicong et al. in 1952.


Lithology and Thickness

Paleosols. It is the lowest formation under the Yuemengou Gr. Lower part consists of lumpy limonite, pyrite or hematite, changing gradually upward into a bauxite layer; Upper part is composed of light-gray to purple-red bauxite shale or bauxite. The thickness is generally 1−10 m, maximum 20 m.


Lithology Pattern: 
Soil


Relationships and Distribution

Lower contact

Unconformable contact with the underlying Ordovician stratum

Upper contact

Disconformable contact with the overlying Benxi Fm

Regional extent

Widespread in various Late Carboniferous sedimentation zones in North China


GeoJSON

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Fossils

Plants Linopteris brongniartii and Neuropteris gigantea in the Zibo Coalfield, and Plants Lepidodendron tripunctatum, L. oculusfelis, L. posthumii, Cathaysiodendron cf. nanpiaoense, etc. in West Henan


Age 

early Late Carboniferous (Lexicon 2017); but Xiangdong Wang et al. (2019, Carboniferous integrative stratigraphy and timescale of China; Science China: Earth Science) diagram it as middle-Late Carboniferous (used here):

Age Span: 

    Beginning stage: 
Moscovian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
315.15

    Ending stage: 
Moscovian

    Fraction up in the ending stage: 
0.3

    Ending date (Ma):  
312.71

Depositional setting

It is interpreted as weathered continental deposits


Depositional pattern:  


Additional Information


Compiler:  

Wang Rennong