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Late Paleozoic to early Triassic multiple roll-back and oroclinal bending of the Mongolia collage in Central Asia
The architecture and mechanics of an orogen can be understood in terms of a system of
collages that are characterized by a complex assemblage of multiple components, but the …
collages that are characterized by a complex assemblage of multiple components, but the …
The timing of India-Asia collision onset–Facts, theories, controversies
The timing of initial collision between India and Asia has remained controversial for half a
century. This paper attempts to review this crucial and hotly debated argument, describing …
century. This paper attempts to review this crucial and hotly debated argument, describing …
[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 …
Highly fractionated Himalayan leucogranites and associated rare-metal mineralization
The formation of the Himalaya was associated with the exhumation of high-grade
metamorphosed rocks of the Higher Himalayan sequence (HHS) complex, which underwent …
metamorphosed rocks of the Higher Himalayan sequence (HHS) complex, which underwent …
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 …
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 …
Raising the Gangdese mountains in southern Tibet
The surface uplift of mountain belts is in large part controlled by the effects of crustal
thickening and mantle dynamic processes (eg, lithospheric delamination or slab breakoff) …
thickening and mantle dynamic processes (eg, lithospheric delamination or slab breakoff) …
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 …
Timing of India‐Asia collision: Geological, biostratigraphic, and palaeomagnetic constraints
A range of ages have been proposed for the timing of India‐Asia collision; the range to some
extent reflects different definitions of collision and methods used to date it. In this paper we …
extent reflects different definitions of collision and methods used to date it. In this paper we …
Processes of initial collision and suturing between India and Asia
The initial collision between Indian and Asian continents marked the starting point for
transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate …
transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate …