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Xiangtang Formation

Xiangtang Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, J2 (TJ26, TJ27b).


Province: 
Gansu, Qinghai

Type Locality and Naming

It was named by Miao Qingxiang as the Xiangtang System in 1954, and was first cited publicly in the 《Regional Stratigraphic Charts of China (draft)》in 1956. The naming section is located in the vicinity of the Xiangtang Village, Minhe County, Qinghai Province, with the profile extending from the Zhu’erzhuang Village to the Mazhuang Village, Yaojie Street of Lanzhou City, Gansu Province serving as its reference section.

Synonym: (享堂组)


Lithology and Thickness

It is composed largely of purple sandstone, gritstone and conglomerate, with a thickness of less than 100 m.


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

Its lower part was cut by fault, and for this reason no base of the formation has been found. Regionally, the next older unit is the Tieyegou Fm or the Muri Fm.

Upper contact

No top found. Regionally, it can be overlain unconformably by the Hekou Gr

Regional extent

The formation is distributed in Minhe and Ledu Counties of Qinghai Province and Lanzhou City and Yongdeng County of Gansu Province. In the Yaojie area of Lanzhou City the formation is composed of grey-green clay, yellow-green sandstone and purple clay, with its basal part consisting of a 7.6m-thick layer of grey-white pebble-bearing sandstone being in a disconformable contact with the grey-green clay from the top part of the underlying Yaojie Fm, with a thickness of 660.7 m. In the area of the Lama Gully, Yongdeng County and the Huishan Mts of Tianzhu County, the lithology of the formation is similar to that found in the Yaojie area, but with a thickness of 252 m in the former area, and with a thickness of only 67.2 m in the latter area. In the Jishiguan area of Minhe County, the rocks of the formation are getting coarser, containing more conglomerates, with a thickness increasing up to 896.8 m.


GeoJSON

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Fossils

In the Xiangtang Gorge the formation is found to yield Chareae fossils such as Euaclistochara yunnanensis, E. nuguishanensis and E. lufengensis var. minor, and yielding also Dinosaur fossils in the Hanjiahu area to the north of Xiangtang as represented by Mamenchisaurus hochuanensis, as well as Crocodilia fossils as represented by Sunosuchus miaoi.


Age 

Schematic strat column suggests late-Middle Jurassic

Age Span: 

    Beginning stage: 
Bathonian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
168.17

    Ending stage: 
Callovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
161.53

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)