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Extending full-plate tectonic models into deep time: Linking the Neoproterozoic and the Phanerozoic
Recent progress in plate tectonic reconstructions has seen models move beyond the
classical idea of continental drift by attempting to reconstruct the full evolving configuration of …
classical idea of continental drift by attempting to reconstruct the full evolving configuration of …
Exploring a lost ocean in the Tibetan Plateau: Birth, growth, and demise of the Bangong-Nujiang Ocean
The vast eastern-Tethyan oceanic domain that throughout the Mesozoic extended between
Gondwana and Eurasia was a puzzle of larger and smaller microcontinents separated by …
Gondwana and Eurasia was a puzzle of larger and smaller microcontinents separated by …
[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …
geological framework and initial growth were fundamentally the result of multiple, previous …
A full-plate global reconstruction of the Neoproterozoic
Neoproterozoic tectonic geography was dominated by the formation of the supercontinent
Rodinia, its break-up and the subsequent amalgamation of Gondwana. The Neoproterozoic …
Rodinia, its break-up and the subsequent amalgamation of Gondwana. The Neoproterozoic …
Tectonic evolution and geodynamics of the Neo-Tethys Ocean
Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …
Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction
Integration of lithostratigraphic, magmatic, and metamorphic data from the Lhasa–Qiangtang
collision zone in central Tibet (including the Bangong suture zone and adjacent regions of …
collision zone in central Tibet (including the Bangong suture zone and adjacent regions of …
Lithospheric architecture of the Lhasa terrane and its control on ore deposits in the Himalayan-Tibetan orogen
Magmatic-hydrothermal ore deposits in collisional orogens are new targets for modern
mineral exploration, yet it is unclear why they preferentially occur in some specific tectonic …
mineral exploration, yet it is unclear why they preferentially occur in some specific tectonic …
The origin and pre-Cenozoic evolution of the Tibetan Plateau
Different hypotheses have been proposed for the origin and pre-Cenozoic evolution of the
Tibetan Plateau as a result of several collision events between a series of Gondwana …
Tibetan Plateau as a result of several collision events between a series of Gondwana …
The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth
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 …
accreted to Eurasia before its collision with the northward drifting Indian continent in the …
Detrital zircon geochronology of pre‐Tertiary strata in the Tibetan‐Himalayan orogen
Detrital zircon data have recently become available from many different portions of the
Tibetan–Himalayan orogen. This study uses 13,441 new or existing U‐Pb ages of zircon …
Tibetan–Himalayan orogen. This study uses 13,441 new or existing U‐Pb ages of zircon …