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Moding Formation

Moding Fm


Period: 
Devonian

Age Interval: 
D13 (63a/21, 64), Emsian (late Early Devonian)


Province: 
Guangxi

Type Locality and Naming

The type section is located at Liujing railway station of Hengxian County, Guangxi. (see Mintang Fm). It was named by Guangxi Team of Regional Geological Survey in 1982. The upper part of the Moding Formation was cut off by a strike fault between Moding Fm and its overlying Najiao Fm in the type section. Therefore, the Wuxiangling section in the Nanning suburb is used for a reference. Unfortunately, this section is not protected owing to large-scale constructions.

[Figure Simplified geological map of Liujing area showing the location of type sections of some lithostratigraphic units (red lines) A-Nagaoling Fm, B-Yukiang Fm, C-Moding Fm, D-Najiao Fm, E-Mintang Fm and Gubi Fm.]


Lithology and Thickness

Chert. It is characterized by the yellow brown thin-bedded siliceous rocks intercalated with medium- to fine-grained crystalline dolomite at base. Several red-brown banded tuffs and cherts 1-2 cm thick, are intercalated within siliceous rocks. Partially it contains lenses of low metamorphic siltstone and fine-grained sandstone. The thickness is 54.9 m.


Lithology Pattern: 
Chert


Relationships and Distribution

Lower contact

In the reference section of Wuxiangling, the Moding Fm is conformable in contact to the underlying Yukiang Fm (Yujiang Fm) with a bed of 40 cm thick dolomite at the base.

Upper contact

The top of the formation is a fault contact with the overlying Najiao Fm; but conformable with the Tanhe Fm in the reference section. The Tanhe Fm, less than 70 m thick, established in Nanning area is also characterized by the siliceous rocks but contains dacryoconarids belonging to Eifelian stage. The similar lithology and fossils with Moding Fm make it difficult to separate the two formations.

Regional extent

It is restrictively distributed in the Nanning area of Guangxi.


GeoJSON

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Fossils

Ammonoids: Anetoceras spp., Erbenoceras sp., Mimagoniatites sp. Dacryoconarids: Nowakia barrandei, N. elegans; and Brachiopods Rostrospirifer spp..


Age 

Middle Emsian (late Early Devonian)

Age Span: 

    Beginning stage: 
Emsian

    Fraction up in beginning stage: 
0.7

    Beginning date (Ma): 
399.16

    Ending stage: 
Emsian

    Fraction up in the ending stage: 
0.45

    Ending date (Ma):  
403.22

Depositional setting

It is interpreted as a basin facies environment.


Depositional pattern:  


Additional Information


Compiler:  

Hongfei Hou