Lhasa terrane to the north

E753968

The Lhasa terrane to the north is a major crustal block in southern Tibet that forms part of the Tibetan Plateau and records the geological history of continental collision between India and Eurasia.

All labels observed (1)

Label Occurrences
Lhasa terrane to the north canonical 1

How this entity was disambiguated

Statements (41)

Predicate Object
instanceOf crustal block ⓘ
geological terrane ⓘ
adjacentTo Himalayan orogenic belt ⓘ
Qiangtang terrane ⓘ
boundedBy Bangong–Nujiang suture zone ⓘ
Yarlung Tsangpo suture zone ⓘ
contains Cenozoic granitoids ⓘ
Mesozoic magmatic arcs ⓘ
sedimentary basins ⓘ
continent Asia ⓘ
formedBy accretion to the Eurasian margin ⓘ
hasElevation high plateau ⓘ
hasEvent Cenozoic uplift ⓘ
India–Asia collision-related deformation ⓘ
Mesozoic magmatic arc development ⓘ
hasGeologicalAge Mesozoic to Cenozoic ⓘ
hasResearchField geochronology ⓘ
paleogeography ⓘ
petrology ⓘ
structural geology ⓘ
tectonics ⓘ
hasRockType granitoid rocks ⓘ
metamorphic rocks ⓘ
sedimentary rocks ⓘ
volcanic rocks ⓘ
hasTectonicActivity Cenozoic crustal thickening ⓘ
strike-slip faulting ⓘ
thrust faulting ⓘ
locatedIn China ⓘ
Tibet Autonomous Region ⓘ
southern Tibet ⓘ
namedAfter Lhasa ⓘ
orogeny Himalayan orogeny ⓘ
partOf Tibetan Plateau ⓘ
recordsProcess continental collision between India and Eurasia ⓘ
separatedFrom Indian plate ⓘ
linked to: India Plate

Qiangtang terrane ⓘ
significantFor evolution of the Tibetan Plateau ⓘ
study of India–Asia collision ⓘ
tectonicSetting collisional orogen ⓘ
underlainBy continental crust ⓘ

How these facts were elicited

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Indus-Tsangpo Suture Zone → boundedBy → Lhasa terrane to the north ⓘ