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Decoupling during continental collision and intra-plate deformation
Dimitrios Sokoutis
*
,
Ernst Willingshofer
*
Corresponding author for this work
non-UU output of (former) DES-UU members
Research Programme in Earth Sciences Utrecht (DES / IVAU)
External unknown
University of Amsterdam
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Keyphrases
Continental Collision
100%
Intraplate Deformation
100%
Weak Zone
100%
Mountain Belts
75%
Subsidence
50%
Intraplate
50%
Modeling Results
50%
Dominant Deformation Mechanisms
50%
Foreland Basin
25%
Strain Partitioning
25%
Continental Lithosphere
25%
Plate Boundary
25%
Plate Coupling
25%
Deformation Mechanism
25%
Model Domain
25%
Initial Geometry
25%
Deformation Phase
25%
Mountain Building
25%
Wedge Shape
25%
Geometric Configuration
25%
Tectonic Boundary
25%
Lithospheric Model
25%
Topographic Evolution
25%
Strain Localization
25%
Triangular Shape
25%
Lateral Capacity
25%
Strength Variation
25%
Geometric Evolution
25%
Strain Control
25%
Weak Parts
25%
Rheologic
25%
Vertical Strain
25%
Earth and Planetary Sciences
Continental Collision
100%
Decoupling
100%
Lithosphere
80%
Deformation Mechanism
60%
Subsidence
40%
Foreland Basin
20%
Tectonics
20%
Strain Partitioning
20%
Continental Lithosphere
20%
Mountain Building
20%