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.

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Observed surface forms (1)

Surface form Occurrences
Lhasa terrane 0

Statements (41)

Predicate Object
instanceOf crustal block
geological terrane
adjacentTo Himalayan orogenic belt NERFINISHED
Qiangtang terrane NERFINISHED
boundedBy Bangong–Nujiang suture zone NERFINISHED
Yarlung Tsangpo suture zone NERFINISHED
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 NERFINISHED
southern Tibet NERFINISHED
namedAfter Lhasa NERFINISHED
orogeny Himalayan orogeny NERFINISHED
partOf Tibetan Plateau NERFINISHED
recordsProcess continental collision between India and Eurasia
separatedFrom Indian plate NERFINISHED
Qiangtang terrane NERFINISHED
significantFor evolution of the Tibetan Plateau
study of India–Asia collision
tectonicSetting collisional orogen
underlainBy continental crust

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