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Mohe Formation

Mohe Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, J2 (TJ8).


Province: 
Heilongjiang

Type Locality and Naming

It was named by the Map Compiler

Jingeng Sha (coordinator) Group under the Chinese Academy of Geological Sciences of the former Ministry of Geology in 1963, and was first cited publicly by the Compiler

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of Heilongjiang Province. The naming section represents the former Wusuli-River section of carbonaceous shale-sandstone association located in the vicinity of the Wusuli River on the right bank of the upper reaches of the Heilong River, with the N35 P12 profile in the Beishan Mts 18 km apart from No. 2 branch line of the Xiufeng Township, Tahe Town serving as its reference section. Upper (second) formation in Emurhe Gr.

Synonym: (漠河组)


Lithology and Thickness

Characterized chiefly by rhythmic sedimentation of yellow-brown and grey-yellow conglomerates, pebble-bearing sandstones, grey-black argillaceous siltstones and carbonaceous shales, with its lower part being intercalated with calcareous and argillaceous siltstones and thin-bedded black-grey microcrystalline limestones, and with its upper part containing tuffaceous conglomerates, carbonaceous mudstones, intercalated with cellular poor-quality coal, with a thickness of over 3550 m.


Lithology Pattern: 
Aus conglomerate


Relationships and Distribution

Lower contact

It is in a conformable contact with the underlying Ershi'erzhan Fm

Upper contact

It is in a conformable contact with the overlying Kaikukang Fm

Regional extent

The formation is distributed largely in the Upper Heilongjiang Depression, and is exposed on the surface in the Jibei area of Xilin County, as well as in a zone extending from the lower reaches of the Dasika River on the west along the Heilong River easterly to the Yongan Railway Station and Guzhan Station east of the Mohe River in the form of a E-W-trending belt. There are found widespread exposures of the formation in the area of the No. 22 Railway Station till the Kakukang Township, the area of the No. 21 Railway Station till the Yixiken region, and at 18 km of the No. 2 Branch Line of Xiufeng Township of Tahe Town, with less changes in its lithology. In 1978 the No. 2 Regional Survey Party of Heilongjiang Province created the Emurhe Formation as a synonym for the formation.


GeoJSON

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Fossils

It yields plant fossils as represented by Podozamites lanceolatus, Raphaelia diamensis, Cladophlebis denticulate, C. argutula, C. cf. raciborskii, Ginkgoites cf. sibiricus and Nilssonia orentals, in addition to Ostracoda, bivalve and Gastropoda fossils.


Age 

Schematic stratigraphic columns suggests Bathonian age.

Age Span: 

    Beginning stage: 
Bathonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
168.17

    Ending stage: 
Bathonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
165.29

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator) Group under the Chinese Academy of Geological Sciences of the former Ministry of Geology in 1963, and was first cited publicly by the Compiler

Jingeng Sha (coordinator) Group for the Regional Stratigraphic Chart of Heilongjiang Province. The naming section represents the former Wusuli-River section of carbonaceous shale-sandstone association located in the vicinity of the Wusuli River on the right bank of the upper reaches of the Heilong River, with the N35 P12 profile in the Beishan Mts 18 km apart from No. 2 branch line of the Xiufeng Township, Tahe Town serving as its reference section. Upper (second) formation in Emurhe Gr.

Synonym: (漠河组)

Lithology and Thickness:

Characterized chiefly by rhythmic sedimentation of yellow-brown and grey-yellow conglomerates, pebble-bearing sandstones, grey-black argillaceous siltstones and carbonaceous shales, with its lower part being intercalated with calcareous and argillaceous siltstones and thin-bedded black-grey microcrystalline limestones, and with its upper part containing tuffaceous conglomerates, carbonaceous mudstones, intercalated with cellular poor-quality coal, with a thickness of over 3550 m.

Lithology-pattern: Aus conglomerate

Relationships and Distribution:

Lower contact:

It is in a conformable contact with the underlying Ershi'erzhan Fm

Upper contact:

It is in a conformable contact with the overlying Kaikukang Fm

Regional extent:

The formation is distributed largely in the Upper Heilongjiang Depression, and is exposed on the surface in the Jibei area of Xilin County, as well as in a zone extending from the lower reaches of the Dasika River on the west along the Heilong River easterly to the Yongan Railway Station and Guzhan Station east of the Mohe River in the form of a E-W-trending belt. There are found widespread exposures of the formation in the area of the No. 22 Railway Station till the Kakukang Township, the area of the No. 21 Railway Station till the Yixiken region, and at 18 km of the No. 2 Branch Line of Xiufeng Township of Tahe Town, with less changes in its lithology. In 1978 the No. 2 Regional Survey Party of Heilongjiang Province created the Emurhe Formation as a synonym for the formation.

GeoJSON:

Fossils:

It yields plant fossils as represented by Podozamites lanceolatus, Raphaelia diamensis, Cladophlebis denticulate, C. argutula, C. cf. raciborskii, Ginkgoites cf. sibiricus and Nilssonia orentals, in addition to Ostracoda, bivalve and Gastropoda fossils.

Age:

Schematic stratigraphic columns suggests Bathonian age.

Age span:

Beginning stage: Bathonian

Fraction up in beginning stage: 0.0

Beginning date (Ma):

Ending stage: Bathonian

Fraction up in ending stage: 1.0

Ending date (Ma):

Depositional setting:

Depositional-pattern:

Additional Information

Compiler

Jingeng Sha (coordinator)