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Jixiangfeng Formation

Jixiangfeng Fm


Period: 
Jurassic

Age Interval: 
Upper Jurassic, J3 (TJ8).


Province: 
Inner Mongolia

Type Locality and Naming

It was named by the No. 2 Regional Survey Party under the Geological Bureau of Heilongjiang Province in 1980, and was first cited publicly by Wang Ying in 1985. The naming section is located on the northern slope of the Qishangfangzi Mts to the north of the Jixiangfeng Railway Station of Yakeshi City, Hulunbar League, Inner Mongolia. Lower (fourth) formation in Xing'anlin Gr.

Synonym: (吉祥峰组)


Lithology and Thickness

It represents a set of dark-colored soda-rich rhyolitic volcanic lava and volcaniclastic strata. The rock types of the formation are represented by basic rhyolite, rhyolitic porphyry, felsitic porphyry, quartz-porphyry, tuffaceous breccia, ignimbrite, volcanic tuff and a small amount of tuffaceous sandy conglomerate.


Lithology Pattern: 
Volcanics


Relationships and Distribution

Lower contact

It is in a conformable contact with the underlying Tamulangou Fm

Upper contact

It is in a conformable contact with the overlying Murui Fm

Regional extent

The formation is distributed at the major peak of the Greater Khingan Mts as well as on the eastern and western slopes of the Greater Khingan. In the area of eastern slope and the major peak of the Greater Khingan the formation consists of an alternating layer of basic rhyolite, dacite, rhyolitic porphyry together with basic rhyolitic ignimbrite and pure ignimbrite, intercalated with a small amount of purple sandstone, with a thickness of 1955.8 m. On the western slope of the above-mentioned mountain the thickness of the formation is smaller. As is seen in the newly created Southwest Hill section on the Shangkuli Farm of the Ergune Right Banner the formation is composed mainly of tuffaceous breccia, ignimbrite and tuffaceous sandy conglomerate, with a thickness of over 100 m. The thickness of the formation on the eastern bank of the Ergune River of the Chenbarhu Banner is as great as 1076 m.


GeoJSON

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Fossils

It yields plant fossils only in western part of the Chenbarhu Banner, as represented by Czekanowskia rigida, Pityophyllum sp., and Phoenicopsis.


Age 

Schematic stratigraphic column suggests a late-Oxfordian age.

Age Span: 

    Beginning stage: 
Oxfordian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
158.16

    Ending stage: 
Oxfordian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
154.78

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)