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Lure Formation

Lure Fm


Period: 
Devonian

Age Interval: 
D21 (40west), Eifelian (Middle Devonian)


Province: 
Gansu

Type Locality and Naming

The type section is located at Dangduogou, 24 km northwest of Têwo County, Gansu Province. It was named by Xi’an Institute of Geology and Mineral Resources and Gansu No 1 Team of Regional Geological Survey in 1973. Qin Fong and Gan Yiyan formally quoted it in 1976.


Lithology and Thickness

Limestone. The formation is composed of gray to dark-gray medium- to thick-bedded fine-grained bioclastic limestone, thin- to medium-bedded calcarenite and dolomitized bioclastic limestone intercalated with limestone, sandy shale and calcareous siltstone. In the middle and upper parts, it is intercalated with multiple layers of reefal facies. It is 238.6 m thick.


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

It conformably overlies the iron-bearing clastic rock of the Dangduo Fm.

Upper contact

It conformably underlies the Xiawuna Fm.

Regional extent

The lithology and thickness of this formation are stable in the west. It is 170-210 m thick from Luqu to Xiawuna and gets slightly thicker to 239 m at Dangduogou. Eastwards at the Yiwagou section, the clastic content of epicontinental origin gradually increases, therefore the thickness can reach up to 812.4 m.


GeoJSON

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Fossils

There are abundant brachiopods and corals, and a few bivalve, gastropod, ostracoda, trilobites and conodonts etc. The Brachiopods can be divided into the Unicinulus subcordiformis-Spissophyllum massivum assemblage zone in the lower part, the Indospirifer-Syringopora eifeliensis assemblage zone in the middle part and the Productella morsovensis-Redstonea kuznetskiensis assemblage zone in the upper part.


Age 

Eifelian (Middle Devonian)

Age Span: 

    Beginning stage: 
Eifelian

    Fraction up in beginning stage: 
0.2

    Beginning date (Ma): 
392.50

    Ending stage: 
Eifelian

    Fraction up in the ending stage: 
0.8

    Ending date (Ma):  
387.10

Depositional setting

The depositional facies sequence from bottom to top is suggested as: open platform, to platform basin, to a semi-restricted platform, then a platform-marginal reef facies.


Depositional pattern:  


Additional Information


Compiler:  

(Cao Xuanduo)