Results 61 to 70 of about 31,153 (271)
TERRAIN TECTONICS OF THE CENTRAL ASIAN FOLDED BELT
The terrain analysis concept envisages primarily a possibility of approximation of fragments / terrains of various geodynamic settings which belong to different plates. The terrain analysis can supplement the theory of plate tectonics in solving problems
M. M. Buslov
doaj +1 more source
Surface and Crustal Response to Deep Subduction Dynamics: Insights From the Apennines, Italy [PDF]
Riccardo Lanari +4 more
openalex +1 more source
ABSTRACT We present novel 3D subsidence data enabling vertical movements' quantification during the early formation of the Pyrenean retro‐wedge. From Cenomanian to Turonian times, subsidence is relatively low (~26 ± 10 m/Myr), corresponding to a brief 10 Myr thermal re‐equilibration of the European lithosphere following the hyperextended rift episode ...
Benoit Issautier +5 more
wiley +1 more source
Onset of double subduction controls plate motion reorganisation
Face-to-face double subduction systems, in which two oceanic plates subduct toward each other, are essential elements of plate tectonics. Two subduction zones in such systems are typically uneven in age and their spatially and temporally variable ...
Kuidi Zhang, Jie Liao, Taras Gerya
doaj +1 more source
Large-scale subduction controls three-dimensional mantle flow beneath the European Alps [PDF]
Frederik Link, Georg Rümpker
openalex +1 more source
In the regime of plate tectonics, the subduction of an oceanic plate generally terminates with the collision and accretion of continental terranes. Then, a new subduction zone may form in the neighboring oceanic plates, which is defined as the terrane ...
Fengyuan Cui, Zhong‐Hai Li
doaj +1 more source
The Iranian plateau is a vast inland region with a smooth average elevation of c. 1.5 km formed at the rear of the Zagros orogen as a result of the Arabia‐Eurasia collision (i.e., over the last 30–35 Myr).
T. François +3 more
doaj +1 more source
Horizontal subduction zones, convergence velocity and the building of the Andes [PDF]
Joseph Martinod +4 more
openalex +1 more source
Frictional Behavior of Input Sediments to the Hikurangi Trench, New Zealand
The Hikurangi subduction zone hosts shallow slow‐slip events, possibly extending to the seafloor. The mechanisms allowing for this behavior are poorly understood but are likely a function of the frictional properties of the downgoing seafloor sediments ...
H. S. Rabinowitz +5 more
doaj +1 more source
Slow slip on the northern Hikurangi subduction interface, New Zealand [PDF]
A Douglas +3 more
openalex +1 more source

