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Geology, ISSN 0091-7613, 08/2013, Volume 41, Issue 8, pp. 911 - 914
Subduction systems are inherently three-dimensional, with significant along-strike variations in the timing and style of deformation and magmatism. Geodynamic... 
GEOLOGY | SUBDUCTION | DYNAMICS | EXTENSION | PLATE | LITHOSPHERE | FLOW | MANTLE | INSIGHTS | FAULTS | Strike-slip faults (Geology) | Subduction zones (Geology) | Research | Geodynamics | Horizontal | Trenches | Mathematical analysis | Lithosphere | Basins | Slabs | Curvature | Failure
Journal Article
Tectonophysics, ISSN 0040-1951, 08/2016, Volume 684, pp. 12 - 22
Analog models of tectonic processes at various scales commonly use silicone polymers to simulate viscous flow in the lower crust and mantle. To achieve dynamic... 
Viscoelasticity | Analog modeling | Silicone polymer | Maxwell model | Rheology | Analog materials | GEOCHEMISTRY & GEOPHYSICS | POLYMERS | CONTINENTAL LITHOSPHERE | BEHAVIOR | FLOW | Earth | Usage | Newton's laws of motion | Analysis | Tectonics (Geology) | Models | Mantle | Silicones | Valuation | Lithosphere | Real property
Journal Article
FRONTIERS IN EARTH SCIENCE, ISSN 2296-6463, 11/2018, Volume 6
Three-dimensional analog experiments are employed to explore how self-sustaining subduction may initiate along an oceanic transform fault. The models include a... 
CONTINENTAL MARGINS | TECTONICS | RETREATING SLABS | lithosphere | STRAIN LOCALIZATION | subduction initiation | serpentinization | analog modeling | FORE-ARC | buoyancy | subduction | GEOSCIENCES, MULTIDISCIPLINARY | DYNAMICS | oceanic fault | DUCTILE SHEAR ZONES | MANTLE FLOW | LABORATORY EXPERIMENTS | Subduction zones (Geology) | Models | Transform faults | Natural history
Journal Article
Geophysical Journal International, ISSN 0956-540X, 08/2008, Volume 174, Issue 2, pp. 719 - 732
Journal Article
Geology, ISSN 0091-7613, 08/2013, Volume 41, Issue 8, pp. 839 - 842
Subduction initiation at passive margins plays a central role in the plate tectonics theory. However, the process by which a passive margin becomes active is... 
Geology | COMPRESSIONAL DEFORMATION | TECTONICS | GEOLOGY | ACTIVE DEFORMATION | PATTERN | FORCE | INITIATION | SEA | INSIGHTS | REGION | Subduction zones (Geology) | Research | Geodynamics | Plate tectonics | Stresses | Southwest | Gibraltar | Oceans | SIM | Migration | Tectonics | Convergence | Earth Sciences | Sciences of the Universe | Physics | Geophysics | Environmental Sciences | Global Changes
Journal Article
Earth and Planetary Science Letters, ISSN 0012-821X, 2008, Volume 271, Issue 1, pp. 226 - 232
Spatial distribution of UHP/LT terrains suggests that their exhumation is essentially a three-dimensional process that occurs only locally in specific sites... 
arc–continent collision | UHP/LT rocks | continental subduction | exhumation | physical thermo-mechanical modelling | arc-continent collision | TECTONICS | MECHANISM | SUBDUCTION | METAMORPHISM | RHEOLOGY | DEFORMATION | GEOCHEMISTRY & GEOPHYSICS | MASSIF | EVOLUTION | CONVERGENCE
Journal Article
Journal of Structural Geology, ISSN 0191-8141, 04/2012, Volume 37, pp. 65 - 74
The cause of upper-crustal segmentation into rhomb-shaped, shear zone-bound domains associated with contractional sedimentary basins in hot, wide orogens is... 
Plateau formation | Basin formation | Analogue modelling | Central Andes | Transpression | Central andes | NW ARGENTINA | TECTONICS | FORE-ARC | MECHANICS | GEOSCIENCES, MULTIDISCIPLINARY | PUNA PLATEAU | SUBDUCTED NAZCA PLATE | NORTHERN CHILE | FAULT ZONE | MAGMATIC EVOLUTION | KINEMATICS | Sedimentary basins | Analysis | Tectonics (Geology)
Journal Article
Earth and Planetary Science Letters, ISSN 0012-821X, 2004, Volume 222, Issue 1, pp. 209 - 216
Journal Article
GEOLOGY, ISSN 0091-7613, 03/2014, Volume 42, Issue 3, pp. E329 - E329
We thank Marques for his Comment (Marques, 2014) on our paper (Duarte et al., 2013) about subduction initiation at the southwest Iberia margin (SIM). Here we... 
GEOLOGY | Earth Sciences | Sciences of the Universe | Geophysics
Journal Article
Journal of Structural Geology, ISSN 0191-8141, 2008, Volume 30, Issue 2, pp. 177 - 193
Journal Article