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Alatag Formation
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Alatag Fm base reconstruction

Alatag Fm


Period: 
Devonian

Age Interval: 
D21 (13,77); early middle Devonian


Province: 
Xinjiang

Type Locality and Naming

Eastern South Tianshan. The type section is located at the eastern slope of Karakzile Mt., south of Kümüx in Tosun County, the Xinjiang Uygur Autonomous Region. It was named by Xinjiang Team of Regional Geological Survey in 1965, and was published by the "Regional Scale of Northwest China-Xinjiang” in 1981.


Lithology and Thickness

Limestone and siliciclastics. The section on the eastern slope of Karakzile Mt. is mainly characterized by gray, grayish-black bioclastic limestone, marble, intercalated with chlorite-sericite-quartz schist, metamorphic sandstone and sandy conglomerate. In the bottom are gray pebble limestone and white marble. The thickness is 6167 m.

In the mountainous area north of Karakzile tag, this formation is composed of crystalline limestone, sandstone, siltstone and chlorite-sericite-quartz schist. The thickness is 2100 to 4000 m.

At the south slope of Klatag, the Formation is composed of detrital limestone, oolitic limestone, sandstone and chert, intercalated with conglomerate. The outcropping thickness is more than 181 m.

In the area south of Kaidu River and north of Sairimu River, the formation is characterized by greywacke intercalated with siltstone, conglomerate. The upper part is composed of limestone and dolomite intercalated with calcareous sandstone. It is 3217 m in thickness.

In the Liushugou-Huolangwote area south of Sa'arming Mt., it is intercalated with intermediate-basic to acidic volcanic clastics. The thickness is 5974.6 m in total.


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

Conformably or disconformably overlies the Aerpishimaibulak Fm [NOT IN LEXICON].

Upper contact

Conformable contact with the overlying Saarming Fm (Sa'arming Fm)

Regional extent

The formation can be recognized on the eastern slope of Karakzile Mt., North of Karaziletag, at the south slope of Klatag, South of Kaidu River and north of Sairimu River and in the Liushugou-Huolangwote area south of Saarming Mt.


GeoJSON

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Fossils

The limestone on the eastern slope of Karakzile Mt.contains coral fossils: Favosites, Pachyfavosites, Heliolites, Emmonsia, and Xystriphyllum.

North of Karaziletag the formation yields coral fossils: Thamnopora incerta, T. ex gr. Tumefacta, Heliolites, Squameofavosites and Pseudamplexus.

At the south slope of Klatag the formation contains coral fossils: Tamnopora cf. reticulata, Wedekindophyllum cf. corneolum.

South of Kaidu River and north of Sairimu River the upper part of the formation contains corals: Disphyllum, Cyathophyllum, Favosites and brachiopods: Camarotoechia, Atrypa.


Age 

early middle Devonian

Age Span: 
S

    Beginning stage: 
Eifelian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
394.30

    Ending stage: 
Eifelian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
385.30

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

(Cao Xuanduo)