Results 61 to 70 of about 31,153 (271)

TERRAIN TECTONICS OF THE CENTRAL ASIAN FOLDED BELT

open access: yesГеодинамика и тектонофизика, 2015
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]

open access: bronze, 2023
Riccardo Lanari   +4 more
openalex   +1 more source

3D Quantification of Subsidence During Pyrenean Retro‐Wedge Initiation: Role of Structural and Thermal Inheritance on Hyperextended Margin Inversion (Aquitaine Basin)

open access: yesTerra Nova, EarlyView.
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

open access: yesNature Communications
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

Terrane Collision‐Induced Subduction Initiation: Mode Selection and Implications for Western Pacific Subduction System

open access: yesGeochemistry, Geophysics, Geosystems
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

Buildup of a dynamically supported orogenic plateau: Numerical modeling of the Zagros/Central Iran case study

open access: yesGeochemistry, Geophysics, Geosystems, 2014
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]

open access: green, 2010
Joseph Martinod   +4 more
openalex   +1 more source

Frictional Behavior of Input Sediments to the Hikurangi Trench, New Zealand

open access: yesGeochemistry, Geophysics, Geosystems, 2018
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

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