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Mole Gr

Mole Gr


Period: 
Triassic

Age Interval: 
Late Triassic, (TJ20)


Province: 
Qinghai

Type Locality and Naming

The named section is located in Datong River Basin, Qinghai Province. A Comparative Study of Multiple Stratigraphic Division in Qinghai Province in 1994 divided the Mole Group into a lower Atasi Fm and an upper Galedesi Fm. This Lexicon follows it.

Synonym: In 1975, the 105 Group of Qinghai Coalfield was named Moeller Group in Datong River Basin. In 1976, the Upper Triassic strata with marine facies or doubtful marine interlayer in the central and southern Qilian Mountains were named as the Moler Group in the "Northwest Division Stratigraphic Conference". In 1983, Yang Zunyi and others established the Ata Temple Group in Ata Si Gou, Yike Wulan Township, Gangchah County, and the Gaede Temple Group in Gaede Temple, Mole Township, Qilian County.


Lithology and Thickness

The lower and upper members of the Atasi Fm (lower formation of the Mole Gr) are composed of gray-white, gray-green, dark purple sandstone, pebbled sandstone and occasionally gray-green or purplish pink siltstone. The upper part consists of grey and dark grey siltstones, silty shale interbedded with carbonaceous shale and sandstone.

Galedesi Fm (upper formation of the Mole Gr) is a rhythmic bed composed of gray, dark gray siltstone, silty shale and gray-light gray sandstone, with carbonaceous shale, coal seam or black shale in some parts. It was a pseudo-conformable contact with the underlying Chelmagou Fm or Junzihe Fm, 1454.31 m thick.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

It has a pseudo-conformable contact with the underlying Chelmagou Fm or Junzihe Fm.

Upper contact

Next younger unit is indicated on schematic strat column as the lower Jurassic Daxigou Gr (Daxigou Fm?); but this TJ20 column has the Xiaomeigou Fm of lower Jurassic as the overlying unit.

Regional extent

The Galedesi Fm is mainly distributed in the western section of the central and southern Qilian Mountains. The lithology is relatively stable in the region and has been damaged by the structure.


GeoJSON

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Fossils

Calamites sp., Paracalamites sp., Danaeopsis fecunda, Taeniocladopsis rhizomoides, Glossophyllum? And the bivalve fossils Unio, Utschamiella longa, etc.


Age 

Tong et al. (2019; Triassic integrative stratigraphy and timescale of China; Science China: Earth Sciences, 82: 189-222) indicate that Galedesi Fm is Norian-Rhaetian and Atasi Fm is Carnian (dashed base).

Age Span: 

    Beginning stage: 
Carnian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
237.00

    Ending stage: 
Rhaetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
201.36

Depositional setting

The Atasi Formation is marine-continental sedimentary facies. The overlying Galedesi Formation is a marshy - lacustrine deposit.


Depositional pattern:  


Additional Information


Compiler:  

Cao Hongsheng, Sun Xin and Tong Jinnan.