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Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation
Despite a long research history over the past 150 years, the geometry, kinematics, and
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …
Propagation of the deformation and growth of the Tibetan–Himalayan orogen: A review
Long-standing problems in the geological evolution of the Tibetan–Himalayan orogen
include where the India–Asia convergence was accommodated and how the plateau grew …
include where the India–Asia convergence was accommodated and how the plateau grew …
[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 …
Gangdese magmatism in southern Tibet and India–Asia convergence since 120 Ma
A compilation of 290 zircon U–Pb ages of intrusive rocks indicates that the Gangdese
Batholith in southern Tibet was emplaced from c. 210 Ma to c. 10 Ma. Two intense magmatic …
Batholith in southern Tibet was emplaced from c. 210 Ma to c. 10 Ma. Two intense magmatic …
Paleocene‐Eocene foreland basin evolution in the Himalaya of southern Tibet and Nepal: Implications for the age of initial India‐Asia collision
Siliciclastic sedimentary rocks derived from the southern Lhasa terrane, sitting depositionally
upon rocks of the northern Indian passive continental margin, provide an estimate of the age …
upon rocks of the northern Indian passive continental margin, provide an estimate of the age …
Cenozoic tectonic evolution of Asia: A preliminary synthesis
Asia has been a major testing ground for various competing models of continental
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
Reconstructing Greater India: Paleogeographic, kinematic, and geodynamic perspectives
Key in understanding the geodynamics governing subduction and orogeny is reconstructing
the paleogeography of 'Greater India', the Indian plate lithosphere that subducted since …
the paleogeography of 'Greater India', the Indian plate lithosphere that subducted since …
Crustal-scale duplexing beneath the Yarlung Zangbo suture in the western Himalaya
The fate of the Indian plate during continental collision with Asian terranes, and the
proportion of the Indian crust that is underthrust or subducted beneath Tibet as opposed to …
proportion of the Indian crust that is underthrust or subducted beneath Tibet as opposed to …
Implications of shortening in the Himalayan fold‐thrust belt for uplift of the Tibetan Plateau
Recent research in the Himalayan fold‐thrust belt provides two new sets of observations that
are crucial to understanding the evolution of the Himalayan‐Tibetan orogenic system. First …
are crucial to understanding the evolution of the Himalayan‐Tibetan orogenic system. First …
Restoration of Cenozoic deformation in Asia and the size of Greater India
A long‐standing problem in the geological evolution of the India‐Asia collision zone is how
and where convergence between India and Asia was accommodated since collision …
and where convergence between India and Asia was accommodated since collision …