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Nanlong Formation

Nanlong Fm


Period: 
Permian

Age Interval: 
P2 (94), Guadalupian Epoch (Middle Permian)


Province: 
Hainan

Type Locality and Naming

The type section is located at the Nanlong Village in the Namu River Valley of Dongfang City, Hainan Province. It was named by the Regional Geological Survey Party of Guangdong Province in 1964.


Lithology and Thickness

Clastics. Composed mainly of a suite of grey-brown, dark-grey and grey-green microclastic rocks, intercalated with carbonate and siliceous rocks. The major rock types are siltstone, siliceous siltstone, fine-grained quartz-sandstone, micro-grained quartz-greywacke, silty calcareous hydromica-bearing siltstone, sandy siltstone, siliceous siltstone and marl. Thickness is about 400 m.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

Conformable contact with the underlying Eding Fm

Upper contact

Uncertain due to incomplete exposure on the surface due to denudation.

Regional extent

Distributed largely in the Changhua River Valley in the Changjiang County of Dongfang City


GeoJSON

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Fossils

Its middle and upper parts yield such Plant fossils (phytolites) as Annularia mucronata, Taeniopteris sp., etc., and with the upper part only yielding the Annularia crassiuscula, Pecopteris arborescens, etc. In the Niudiling section the Nanlong Fm is 350-m thick, with its upper part yielding Fusulinida represented by Parafusulina bosei, Parafusulina sp.; brachiopods such as Leptodus nobilis, L. richthofeni, etc.; and bivalves such as Nuculopsis sp., Ensipteria sp., etc., and with its top part yielding Cephalopoda represented by Shouchangoceras shouchangense, Altudoceras orientale, etc.


Age 

In the Namu River Valley, the age of the formation is so far uncertain whether it belongs to the Maokou’an Stage or to the Wuchiapingian Stage, or to the combined Maokouian -Wuchiapingian stages, because of the different views on the recognition of the plant fossils (phytolites) that it yields. The Nanlong Fm in the Niudi Ridge area yields the Kufengian-Stage [mid-Guadalupian Epoch (mid-Middle Permian)] Fusulinida fauna represented by Parafusulina bosei--P. spp. and the ammonoid fauna represented by Shouchangoceras-Altudoceras of the Lengwu’an Stage, [=Capitanian Stage (late Guadalupian Epoch; late-Middle Permian)] indicating that the middle and upper parts of the Nanlong Fm in this particular section belong to the deposits of the Maokou’an Subepoch [=Guadalupian Epoch (Middle Permian)].

Age Span: 

    Beginning stage: 
Kungurian

    Fraction up in beginning stage: 
0.75

    Beginning date (Ma): 
276.60

    Ending stage: 
Capitanian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
259.55

Depositional setting

It is interpreted as littoral-basin facies and coastal-lagoon facies deposits.


Depositional pattern:  


Additional Information


Compiler:  

Xu Guuanghong