Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Xiaochaka Gr

Xiaochaka Gr


Period: 
Triassic

Age Interval: 
Late Triassic, (TJ30a)


Province: 
Xizang (Tibet)

Type Locality and Naming

The type section is located in Xiaochaka, Shenzha County, Tibet. It was named by the Tibet regional geological survey team in 1985 and first publicly cited by Rao Rongbiao et al in 1987.

Synonym: Xocaka Gr, Xiaochaka Fm (spellings). Xiaorongka Group (as used in Jurassic Lexicon entry for the overlying formation); In 1985, Wu Ruizhong et al. named the Upper Triassic in the northern Qiangtang as the Juhuashan Fm, taking the Juhuashan section east of the Gomuxue Mountain in the Shuanghu area of Tibet as the named section, which has the same meaning with this group.


Lithology and Thickness

This group consists of carbonates and clastic rocks. Lower part is gray thick limestone, black limestone and marl, 315 m thick. Upper part is a rhythmic layer of gray, gray-green, brown-yellow and other variegated coarse sandstone, fine sandstone, sandy shale and marl with a thickness of 1163 m.


Lithology Pattern: 
Sandy limestone


Relationships and Distribution

Lower contact

The basal thick-layered limestone of the Xiaochaka Gr is in conformable contact to the underlying top-most sandstone of Kangnan Fm

Upper contact

The limestone and marl at the top are in conformable contact with the overlying Yellow Mudstone of the Lower Jurassic (= probably the lower part of Qushai Fm ?).

Regional extent

The Group is distributed in the north of Shenza County and the south of Ruolagang in Tibet. In the area of Xiaorongka, Beinuocuo, Laxongcuo and Changliangshan in Shenzha, the group overlaps on different strata of Paleozoic and is in pseudo-conformable contact with the overlying Jurassic strata. The lithology can be divided into lower limestone, a middle-variegated sandstone and an upper bioclastic limestone, with a total thickness of 2500-3580 m.


GeoJSON

null

Fossils

The lower part contains bivalves Palaeocardita langlongensis, Entolium cf. quotidianum, Indopecten sp., I. serpaticostus, Plagiostoma nuitoense; Brachiopods: Amphiclina intermedia, A. taurica, Rhaetinopsis pentagonnalis, etc; Corals: Thecosmilia sp.


Age 

Schematic stratigraphic section indicates spanning entire Late Triassic.

Age Span: 

    Beginning stage: 
Carnian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
237.00

    Ending stage: 
Rhaetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
201.36

Depositional setting

It is interpreted as shallow Marine environment.


Depositional pattern:  


Additional Information


Compiler:  

Zhang Shunxin, Zhang Shiyan and Tong Jinnan.