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
Danshuihe Formation

Danshuihe Fm


Period: 
Jurassic

Age Interval: 
Upper Jurassic, (TJ29)


Province: 
Xizang (Tibet)

Type Locality and Naming

It was named by the Regional Survey Party under the Tibetan Geological Bureau in 1987. The naming section is located in the area of Danshui River northeast of Duoma District, Ritu County, Tibet (E 80o26, N 33o40), with its reference section being situated on the western bank of the Bairebu Co to the northwest of the Cabu District, Gaize County, Tibet (E 83°10′, N 34°55′). Schematic strat column in previous "red Chinese Lexicon" suggests it is the upper formation in the Yanshiping Gr and coeval with the Bailongbinghe Fm.

Synonym: (淡水河组)


Lithology and Thickness

Composed of grey medium-, and thin-bedded microcrystal limestone and light-purple brecciated limestone. It is 1293.66 m thick.


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

It is in a conformable contact and partly coeval with the Bailongbinghe Fm

Upper contact

No information given. Regionally, it is unconformably underlying Cenozoic red beds and volcanic rocks.

Regional extent

The formation is found to be exposed only in the Duoma District, Ritu County and on the western bank of Bairebu Co, Gaize County, Tibet, with a consistent lithology and an exposed thickness of over 1250 m. Coeval with the Bailongbinghe Fm in this same location.


GeoJSON

null

Fossils

In the Duoma area it yields bivalves Pleuromya cf. spitiensis, etc.; and gastropods as represented by Elegantella sp. cf., E. conoidalis, Monoplocus sp.; while in the area of the western bank of the Bairebu Co it yields coral fossils Schizosmilia rollieri, Dermoseris delogaboi, D. doblogana and Montlivaltia bifibra.


Age 

Schematic strat column in previous "red Chinese Lexicon" had implied that the Danshuihe Fm spanned the Late Jurassic. However, because it is coeval with the Bailongbinghe Fm in this same location, then for graphic purposes, it is shown as late-Late Jurassic.

Age Span: 

    Beginning stage: 
Kimmeridgian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
152.01

    Ending stage: 
Tithonian

    Fraction up in the ending stage: 
0.0

    Ending date (Ma):  
149.24

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)