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TuotuoheJur Formation

TuotuoheJur Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, (TJ31)


Province: 
Qinghai

Type Locality and Naming

It was named by Bai Hiasheng in 1989. The naming section is located at Yanshiping by the Qinghai-Tibet Highway in Qinghai Province, with its reference section being situated at 7 km southeast of the Quemoco of Tanggula Township, Germu (Golmud) City, Qinghai Province (Regional Survey Party of Qinghai Province, 1987). Schematic strat column in previous "red Chinese Lexicon" suggests it is the upper-lower formation in the Yanshiping Gr.

Synonym: (沱沱河组); The Tuotuohe Formation is regarded as the synonym of the Buqu Fm, and this Tuotuohe Fm name has been assigned to a Paleocene lithostratigraphic unit in this same Golmund City region by Bureau of Geology and Mineral Resources of Qinghai Province (1997); therefore, the suffix-qualifier of "Jur" was added in this Lexicon to avoid overlap.


Lithology and Thickness

The formation represents alternating layers of grey-violet medium-, and thick-bedded sandstones in association with grey-green medium-, and thick-bedded quartz-siltstones, intercalated with grey and grey-white quartz-sandstones, calico-ferruginous siltstones, grey-black bio-limestones and marls, with a thickness of 1283 m at Yanshiping, and of 530 m in the Quemoco area.


Lithology Pattern: 
Fine-grained sandstone


Relationships and Distribution

Lower contact

Its basal part with its micro-conglomerate is in a conformable contact with the grey-green and violet siltstone and mudstone from the top part of the underlying Qoimaco Fm (Quemocuo Fm).

Upper contact

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

Regional extent

The formation is distributed extensively in the upper reaches of the Tuotuo River, with a consistent thickness.


GeoJSON

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Fossils

In the middle and lower parts of the Yanshiping section the aspect of the contained bivalve fossils is similar to that from the Quemoco Formation, and of the Brachiopod fossils there occur such members of the Bajocian stage as Monsardithyris rauzevauxi, Sphenorhynchia matisconensis and etc., with the upper part of the section being rich in bivalves of the early Bathonian stage such as Isognomon (Mytiloperna) murchisoni, I. (M.) bathonica, Emiodon angulatus, Astarte oolitharum and Protocardia stricklandi, as well as Brachiopod fossils as represented by Burmirhynchia gutta and Holcothyria subovalis.


Age 

Schematic strat column in previous "red Chinese Lexicon" had implied that the TuotuoheJur Fm spanned the Bajocian.

Age Span: 

    Beginning stage: 
Bajocian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
170.90

    Ending stage: 
Bajocian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
168.17

Depositional setting

It represents normal shallow-sea deposits.


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)