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Xiaomeigou Formation

Xiaomeigou Fm


Period: 
Jurassic

Age Interval: 
Early Jurassic, (TJ20, TJ21)


Province: 
Qinghai

Type Locality and Naming

It was named by Yang Fan, Di Hengshu in 1972, and was first cited publicly by the Compiler

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of Qinghai Province in 1980. The naming section is located in the area extending from the Xiaomeigou Gully to the Dameigou Gully about 80 km east of the Taglagan, Qinghai Province.

Synonym: (小煤沟组)


Lithology and Thickness

Lower part is composed largely of grey-yellow, yellow-green and purple conglomerate, sandy conglomerate and pebble-bearing gritstone, intercalated with a small amount of grey and grey-black siltstone, claystone and carbonaceous shale, containing basal conglomerate with a thickness of 29 m. Middle part is grey-yellow, yellowish-pink and grey-white sandstone, siltstone and pebble-bearing sandstone, intercalated with a small amount of claystone and a thick coal layer (11.6 m thick), with a thickness of 89 m. Upper part is mainly of brown-black and grey-black oil shale and shale, intercalated with grey and grey-yellow fine-grained sandstone, siltstone, medium- and coarse-grained sandstones and coal seams, with a thickness of 82 m. The total thickness is 200 m.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

It overlies unconformably the paleo-Proterozoic Kendaban Gr in type region; but regionally, the next older unit is the upper Triassic Galedesi Fm (uppermost formation in Mole Gr).

Upper contact

Regionally, the schematic strat column indicates the next younger unit as Dameigou Fm

Regional extent

The formation is known so far to be distributed only in the Xiaomeigou Gully area on the northern margin of the Chaidamu Basin.


GeoJSON

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Fossils

The lower, middle and upper parts of the formation are found to yield plant fossils key members of which comprise Neocalamites carcinoides, N. nathorsti, Cladophlebis ingens, Cl. nebbensis, Cl. denticulate, Todites williamsoni, Hausmannia ussuriensis, Ginkgoites ferganensis, Pityophyllum longifolium, Czekanowskia elegans and etc.


Age 

Schematic stratigraphic column assigns as Early Jurassic.

Age Span: 

    Beginning stage: 
Hettangian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
201.36

    Ending stage: 
Toarcian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
174.70

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of Qinghai Province in 1980. The naming section is located in the area extending from the Xiaomeigou Gully to the Dameigou Gully about 80 km east of the Taglagan, Qinghai Province.

Synonym: (小煤沟组)

Lithology and Thickness:

Lower part is composed largely of grey-yellow, yellow-green and purple conglomerate, sandy conglomerate and pebble-bearing gritstone, intercalated with a small amount of grey and grey-black siltstone, claystone and carbonaceous shale, containing basal conglomerate with a thickness of 29 m. Middle part is grey-yellow, yellowish-pink and grey-white sandstone, siltstone and pebble-bearing sandstone, intercalated with a small amount of claystone and a thick coal layer (11.6 m thick), with a thickness of 89 m. Upper part is mainly of brown-black and grey-black oil shale and shale, intercalated with grey and grey-yellow fine-grained sandstone, siltstone, medium- and coarse-grained sandstones and coal seams, with a thickness of 82 m. The total thickness is 200 m.

Lithology-pattern: Clayey sandstone

Relationships and Distribution:

Lower contact:

It overlies unconformably the paleo-Proterozoic Kendaban Gr in type region; but regionally, the next older unit is the upper Triassic Galedesi Fm (uppermost formation in Mole Gr).

Upper contact:

Regionally, the schematic strat column indicates the next younger unit as Dameigou Fm

Regional extent:

The formation is known so far to be distributed only in the Xiaomeigou Gully area on the northern margin of the Chaidamu Basin.

GeoJSON:

Fossils:

The lower, middle and upper parts of the formation are found to yield plant fossils key members of which comprise Neocalamites carcinoides, N. nathorsti, Cladophlebis ingens, Cl. nebbensis, Cl. denticulate, Todites williamsoni, Hausmannia ussuriensis, Ginkgoites ferganensis, Pityophyllum longifolium, Czekanowskia elegans and etc.

Age:

Schematic stratigraphic column assigns as Early Jurassic.

Age span:

Beginning stage: Hettangian

Fraction up in beginning stage: 0.0

Beginning date (Ma):

Ending stage: Toarcian

Fraction up in ending stage: 1.0

Ending date (Ma):

Depositional setting:

Depositional-pattern:

Additional Information

Compiler

Jingeng Sha (coordinator)