The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth
Volume: 301, Issue: 1-2, Pages: 241 - 255
Published: Jan 1, 2011
Abstract
The Lhasa Terrane in southern Tibet has long been accepted as the last geological block accreted to Eurasia before its collision with the northward drifting Indian continent in the Cenozoic, but its lithospheric architecture, drift and growth histories and the nature of its northern suture with Eurasia via the Qiangtang Terrane remain enigmatic. Using zircon in situ U–Pb and Lu–Hf isotopic and bulk-rock geochemical data of Mesozoic–Early...
Paper Details
Title
The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth
Published Date
Jan 1, 2011
Volume
301
Issue
1-2
Pages
241 - 255
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