The nature and timing of crustal thickening in Southern Tibet

Geochemical and zircon Hf isotopic constraints from postcollisional adakites

Sun Lin Chung, Mei Fei Chu, Jianqing Ji, Suzanne Y. O'Reilly, N. J. Pearson, Dunyi Liu, Tung-Yi Lee, Ching Hua Lo

Research output: Contribution to journalArticle

281 Citations (Scopus)

Abstract

Rising as "the roof of the world" the Tibetan plateau is now underlain with the thickest continental crust on Earth. How and when was this crust formed, which would have exerted pivotal controls to the formation of the plateau, has long been an issue of hot debates. This paper reports zircon U-Pb ages and Hf isotope data for postcollisional (~ 30-9 Ma) adakites in the southern Lhasa terrane, southern Tibet. A comparative analysis of whole-rock rare earth element geochemistry and zircon Hf isotopes between the adakites and associated Gangdese igneous rocks suggests that the Tibetan crust underwent a major phase of tectonic thickening between ca. 45 and 30 Ma in the region. The lower part of the thickened crust consisted prevailingly of mafic lithologies, which we argue to have resulted from intense basaltic underplating and subsequent remelting that took place during the Late Cretaceous and Eocene time related to the Neotethyan subduction processes including breakoff of the subducted slab at ca. 50 Ma in the early stage of the India-Asia collision. These processes were responsible for not only the juvenile crust formation but also for the creation of a thermally softened lithosphere in the southern Lhasa terrane. The indentation of India, consequently, caused distributed lithospheric thickening with formation of an orogenic root beneath southern Tibet. Root foundering during the Oligocene gave rise to the adakitic magmatism, regional topographic uplift, and onset of northward underthrusting of the Indian plate that has since played a key role in forming the entire Tibetan plateau.

Original languageEnglish
Pages (from-to)36-48
Number of pages13
JournalTectonophysics
Volume477
Issue number1-2
DOIs
Publication statusPublished - 2009 Nov 1

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Tibet
crustal thickening
crusts
zircon
time measurement
crust
plateau
plateaus
terrane
India
isotope
isotopes
indentation
Indian plate
underplating
igneous rock
roofs
igneous rocks
continental crust
roof

Keywords

  • Basaltic underplating
  • Crustal thickening
  • India-Asia collision
  • Neotethyan subduction
  • Postcollisional adakite
  • Tibet

ASJC Scopus subject areas

  • Geophysics
  • Earth-Surface Processes

Cite this

The nature and timing of crustal thickening in Southern Tibet : Geochemical and zircon Hf isotopic constraints from postcollisional adakites. / Chung, Sun Lin; Chu, Mei Fei; Ji, Jianqing; O'Reilly, Suzanne Y.; Pearson, N. J.; Liu, Dunyi; Lee, Tung-Yi; Lo, Ching Hua.

In: Tectonophysics, Vol. 477, No. 1-2, 01.11.2009, p. 36-48.

Research output: Contribution to journalArticle

Chung, Sun Lin ; Chu, Mei Fei ; Ji, Jianqing ; O'Reilly, Suzanne Y. ; Pearson, N. J. ; Liu, Dunyi ; Lee, Tung-Yi ; Lo, Ching Hua. / The nature and timing of crustal thickening in Southern Tibet : Geochemical and zircon Hf isotopic constraints from postcollisional adakites. In: Tectonophysics. 2009 ; Vol. 477, No. 1-2. pp. 36-48.
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