Direct structural evidence of Indian continental subduction beneath Myanmar. [PDF]
Indian continental subduction can explain crustal deformation, magmatic activity and uplift of the Tibetan Plateau following collision, however, the nature of the Indian subducting slab beneath Myanmar and the related tectonic regime remain unclear. Here,
Zheng T +8 more
europepmc +5 more sources
Evidence for a serpentinized plate interface favouring continental subduction. [PDF]
The dynamics of continental subduction is largely controlled by the rheological properties of rocks involved along the subduction channel. Here, the authors reveal a prominent, yet previously undetected, low-velocity body beneath the Western Alps, along ...
Zhao L +12 more
europepmc +8 more sources
How mantle heterogeneities drive continental subduction and magmatism in the Apennines. [PDF]
Petrologic and geophysical observations floored the paradigm shift on the subduction of the continental lithosphere. In long-lived collisional boundaries like the Alpine Himalaya belt, portions of continental lithosphere are pushed down to great depths ...
Giacomuzzi G, De Gori P, Chiarabba C.
europepmc +2 more sources
Mode of intracontinental mountain building controlled by lower crustal composition and mantle lithosphere depletion. [PDF]
Tectonic plate convergence is accommodated across the continental lithosphere via discrete lithospheric subduction or distributed shortening and thickening.
Xu X +14 more
europepmc +2 more sources
Redox state of subducted sediments controls porphyry copper mineralization along the Tethyan belt. [PDF]
The Tethyan orogenic belt hosts numerous world-class porphyry copper deposits, with most forming during the Cenozoic continental collision and fewer during earlier Mesozoic subduction.
Li H, Yang Z, Lu Y, Hou Z.
europepmc +2 more sources
Tectono-sedimentary evolution of the NE Dinarides margin during the Cretaceous Adria-Europe convergence [PDF]
The Cretaceous sedimentation along the NE Dinarides margin occurred in basins above the Europe-dipping Neotethyan Sava subduction zone positioned between Adria- and Europe-derived continental units.
Stojadinović Uroš, Krstekanić Nemanja
doaj +1 more source
Determination of the double-layer structure in orogenic belts and its geological significance
At present, the study of accretionary orogenic belts and collisional orogenic belts has achieved numerous insights and improvements. However, continental subduction, which often occurs during the oceanic and continental transition, has not received ...
WANG Genhou +3 more
doaj +1 more source
The thermal structure of the continental subduction zone can be deduced from high-pressure and ultra-high-pressure rock samples or numerical simulation. However, petrological data indicate that the temperature of subducted continental plates is generally
Ting Luo, Wei Leng
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The role of continental lithospheric thermal structure in the evolution of orogenic systems: application to the Himalayan–Tibetan collision zone [PDF]
Continental collision is a crucial process in plate tectonics. However, in terms of the evolution and the controlling parameters of its lateral heterogeneity, our understanding of the tectonic complexities at such a convergent plate boundary remains ...
M. Liu, D. Yang, R. Qi
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Interplay between oceanic subduction and continental collision in building continental crust
AbstractGeneration of continental crust in collision zones reflect the interplay between oceanic subduction and continental collision. The Gangdese continental crust in southern Tibet developed during subduction of the Neo-Tethyan oceanic slab in the Mesozoic prior to reworking during the India-Asia collision in the Cenozoic.
Di-Cheng Zhu +8 more
openaire +3 more sources

