Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record

Hao Yang Lee, Sun Lin Chung, Ching Hua Lo, Jianqing Ji, Tung Yi Lee, Qing Qian, Qi Zhang

Research output: Contribution to journalArticle

252 Citations (Scopus)

Abstract

Formation of the Linzizong volcanic successions in the Lhasa terrane, southern Tibet has long been related to northward subduction of the Neotethyan oceanic slab under Asia. Here we report new 40Ar/39Ar age results for the volcanic rocks recovered from a large area (29°N to 32°N and 85°E to 93°E) that, together with literature data, delineate two discrete stages of volcanism. These are a widespread Cretaceous stage and an intense, but spatially confined, Paleogene stage. The latter, occurring only in the southern part of the Lhasa terrane, resulted in the Linzizong volcanic successions. Our data, furthermore, suggest southward migration and intensification of the volcanism in the Lhasa terrane with magmatic "flare-ups" at ca. 50 Ma. While the volcanic successions consist dominantly of calc-alkaline rocks typical of arc lava geochemistry, those formed during the flare-up period show significant compositional variations from low-K tholeiitic through calc-alkaline to shoshonitic magma suites. These observations enable us to interpret the volcanic southward migration and following flare-ups as the consequences of rollback and breakoff of the subducted Neotethyan slab that occurred ahead and in the early stage, respectively, of the India-Asia collision. Our interpretation that involves a major Eocene tectonomagmatic activity, and concomitant topographic uplift, in southern Tibet is consistent with Himalayan metamorphic constraints, regional sedimentary records and seismic tomography. Crown

Original languageEnglish
Pages (from-to)20-35
Number of pages16
JournalTectonophysics
Volume477
Issue number1-2
DOIs
Publication statusPublished - 2009 Nov 1

Fingerprint

Tibet
volcanology
terrane
slab
Eocene
slabs
volcanism
flares
calc alkaline rock
seismic tomography
lava
Paleogene
rocks
volcanic rock
subduction
collision
uplift
geochemistry
magma
Cretaceous

Keywords

  • India-Asia collision
  • Linzizong volcanism
  • Neotethyan subduction
  • Slab breakoff
  • Tibet

ASJC Scopus subject areas

  • Geophysics
  • Earth-Surface Processes

Cite this

Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record. / Lee, Hao Yang; Chung, Sun Lin; Lo, Ching Hua; Ji, Jianqing; Lee, Tung Yi; Qian, Qing; Zhang, Qi.

In: Tectonophysics, Vol. 477, No. 1-2, 01.11.2009, p. 20-35.

Research output: Contribution to journalArticle

Lee, Hao Yang ; Chung, Sun Lin ; Lo, Ching Hua ; Ji, Jianqing ; Lee, Tung Yi ; Qian, Qing ; Zhang, Qi. / Eocene Neotethyan slab breakoff in southern Tibet inferred from the Linzizong volcanic record. In: Tectonophysics. 2009 ; Vol. 477, No. 1-2. pp. 20-35.
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AU - Qian, Qing

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AB - Formation of the Linzizong volcanic successions in the Lhasa terrane, southern Tibet has long been related to northward subduction of the Neotethyan oceanic slab under Asia. Here we report new 40Ar/39Ar age results for the volcanic rocks recovered from a large area (29°N to 32°N and 85°E to 93°E) that, together with literature data, delineate two discrete stages of volcanism. These are a widespread Cretaceous stage and an intense, but spatially confined, Paleogene stage. The latter, occurring only in the southern part of the Lhasa terrane, resulted in the Linzizong volcanic successions. Our data, furthermore, suggest southward migration and intensification of the volcanism in the Lhasa terrane with magmatic "flare-ups" at ca. 50 Ma. While the volcanic successions consist dominantly of calc-alkaline rocks typical of arc lava geochemistry, those formed during the flare-up period show significant compositional variations from low-K tholeiitic through calc-alkaline to shoshonitic magma suites. These observations enable us to interpret the volcanic southward migration and following flare-ups as the consequences of rollback and breakoff of the subducted Neotethyan slab that occurred ahead and in the early stage, respectively, of the India-Asia collision. Our interpretation that involves a major Eocene tectonomagmatic activity, and concomitant topographic uplift, in southern Tibet is consistent with Himalayan metamorphic constraints, regional sedimentary records and seismic tomography. Crown

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