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
Germig Formation

Germig Fm


Period: 
Triassic, Jurassic

Age Interval: 
latest Rhaetian-Hettangian (TJ46)


Province: 
Xizang (Tibet)

Type Locality and Naming

"The type locality of the Germig Formation lies 2.5 km south of the small village of Germig and 1.5 km south-southeast of the settlement Nian Duo Cun, near milestone 5260 of the Sino-Nepal International Road (28°42.0'N, 86°08.5'E)." North of Nyalam, and west of Tingri.

Synonym:


Lithology and Thickness

"Chiefly of siltstones and fine-grained sandstones characterized frequently by ripple-bedding.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

Next older unit is the Norian-Rhaetian Derirong Fm.

Upper contact

Regionally, the next younger unit is the Jurassic Pupuga Fm.

Regional extent

Germig Formation crops out in the Lanongla region of southern Tibet, on the northern flank of the Tibetan Himalaya.


GeoJSON

null

Fossils

Hautman et al. (2008) cite Hallam et al (Hallam, A., Wignall, P.B., Yin, J., and Riding, J.B., 2000, An investigation into possible facies changes across the Triassic-Jurassic boundary in southern Tibet: Sedimentary Geology, 137: 101–106.) that it spans part of the Marshi ammonoid zone of latest Rhaetian, and the Tibeticum Zone and part of the Caliphylium ammonite zones of early Hettangian; and they record numerous bivalves.


Age 

Tong et al. (2019, Triassic integrated stratigraphy and timescale in China, Science China: Earth Sciences, v. 62, no. 1) assign it as spanning the latest Rhaetian to early Hettangian.

Age Span: 

    Beginning stage: 
Rhaetian

    Fraction up in beginning stage: 
0.9

    Beginning date (Ma): 
201.80

    Ending stage: 
Hettangian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
200.41

Depositional setting

"As a part of the Tethyan Himalayan tectonic province, the Germig Formation was deposited at the southeastern margin of the Tethys at 25S paleolatitude (Metcalfe, 1996). Deposition was in a shallow, fully marine setting (Hallam et al., 2000)."


Depositional pattern:  


Additional Information


Compiler:  

Mainly extracted from: Hautmann, M; Stiller, F; Cai, H; Sha, J (2008). Extinction-recovery pattern of level-bottom faunas across the Triassic-Jurassic boundary in Tibet: implications for potential killing mechanisms. Palaios, 23(10): 711-718. DOI: https://doi.org/10.2110/palo.2008.p08-005.