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Xiajiabula Gr

Xiajiabula Gr


Period: 
Jurassic

Age Interval: 
Late Jurassic-Early Cretaceous, (TJ47c)


Province: 
Xizang (Tibet)

Type Locality and Naming

It was named by the Coalfields Prospecting Party under the Geological Bureau of Tibet in 1958. The naming section is located at North Gully of Jiabula, Longma Region, Jiangzi County, Tibet (Liu Guifang, 1983), with its reference section being situated at the Yongyang Village (Weimei Village) on the northern bank of the Renlapu River about 20 km northeast of the Jiangzu County town (Wang Yigang and others, 1980).

Synonym: (下加不拉群), Jiabula Fm


Lithology and Thickness

Lower and Middle parts of the group are composed of yellow-green siltstones and grey and dark-grey silty shales, intercalated with limestone lenses, with its basal part being composed of grey-white quartz-sandstone. Upper part is composed of black-dark grey thin-bedded shales, argillaceous siltstone and sand-, iron-, and silica-rich concretions. The thickness is 376 m.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

It is in conformable contact onto the shallow-marine marl of the Weimei Fm.

Upper contact

Its top part being in a conformable contact with the basal grey-black sandy shale intercalated with argillaceous concretions of the Shangjiabula Gr (Sangxiu Fm is lowest formation; but apparently the lower volcanics of that Sangxiu Fm is lacking here?)

Regional extent

The formation is characterized by a consistent lithology, and is distributed extensively in the Jiangzi-Sajia region, as well as in the Changguo-Xiaga region of Sage County in western Tibet, with a greatly varying thickness, being of about 800-2000 m.


GeoJSON

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Fossils

In the North Gully of the Jiabular area the formation yields such ammonite fossils as Spiticeras spitiense, Himalayites stoliczkai, H. seideli, Euthymiceras sp., Berriasella sp., Neocomites sp., Phylloceras sp., Paraboliceras sp., Blanfordiceras sp., Virgatosphinctes sp. and Haplophylloceras strigile; and bivalve fossils such as Buchia spitiensis grandensis, Astarte spitiense, Pleuromya spitiensis and Entolium manggiongense. In the Weimei area it yields such ammonite fossils as Himalayites sp., Berriasella sp., Haplophylloceras sp. and H. strigile.


Age 

Bureau of Geology and Mineral Resources of Tibet Autonomous Region (1997) changed the Xiajiabula Gr into formation and regarded its geological age as Cretaceous. According to the contact relationship with the underlying Weimei Fm and the fossils in the latter (Li et al., 2013), the geological age of Cretaceous is supported. Schematic strat column in previous "red Chinese Lexicon" had implied that the Xiajiabula Gr spanned the Late Jurassic and into Cretaceous. [Ammonites of underlying Weimei Fm would suggest limited to latest-Late Jurassic into Cretaceous.]

Age Span: 

    Beginning stage: 
Tithonian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
146.17

    Ending stage: 
Valanginian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
132.60

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)