Journal article icon

Journal article

Late Triassic orogenic assembly of the Tibetan Plateau: constraints from magmatism and metamorphism in the East Lhasa terrane

Abstract:
The early Mesozoic evolution of the Lhasa terrane, which represents a major component of the Himalayan-Tibetan orogen, remains highly controversial. In particular, geological units and events documented either side of the eastern Himalayan syntaxis (EHS) are poorly correlated. Here, we report new petrological, geochemical and geochronological data for cogenetic peraluminous S-type granites and metamorphic rocks (gneiss and schist) from the Motuo-Bomi-Chayu region of the eastern Lhasa terrane, located on the eastern flank of the EHS. Zircon U-Pb dating indicates that these units record both Late Triassic magmatic (216-206 Ma) and metamorphic (209-198 Ma) episodes. The granites were derived from a Paleoproterozoic crustal source with negative zircon ϵHf(t) values (-5·5 to -16·6) and TDM2 model ages of 1·51-1·99 Ga, and are interpreted to have formed by crustal anatexis of nearby metasediments during collisional orogeny and crustal thickening. The gneisses and schists experienced similar upper amphibolite-facies peak metamorphism and associated partial melting, followed by decompressional cooling and retrograde metamorphism. These rocks were buried to lower-crustal depths and then exhumed to the surface in a collisional orogenic setting during plate convergence. From comparison of these data with those for other metamorphic belts with similar grades and ages, and association of coeval granitic magmatism widespread in the central-east Lhasa terrane, we propose that the studied cogenetic magmatism and metamorphism in the Motuo-Bomi-Chayu region records Late Triassic accretion of the North Lhasa and South Lhasa terranes, which represents the first evidence of the Paleo-Tethys Ocean closure in this part of Asia. These data provide new constraints on the spatial and temporal evolution of the Paleo-Tethyan Wilson Cycle and provide a 'missing link' to correlate the geology and tectonic history of the Lhasa terrane continental crust on either side of the EHS.
Publication status:
Published
Peer review status:
Peer reviewed

Actions


Access Document


Files:
Publisher copy:
10.1093/petrology/egab032

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author


Publisher:
Oxford University Press
Journal:
Journal of Petrology More from this journal
Volume:
62
Issue:
6
Article number:
egab032
Publication date:
2021-04-09
Acceptance date:
2021-04-04
DOI:
EISSN:
1460-2415
ISSN:
0022-3530


Language:
English
Pubs id:
1191989
Local pid:
pubs:1191989
Deposit date:
2024-04-26

Terms of use



Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP