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Continental collision
Two Contrasting Phanerozoic Orogenic Systems Revealed by Hafnium Isotope Data William J
Post-Collisional Formation of the Alpine Foreland Rifts
Collision Orogeny
Subduction and Continental Collision in the Lufilian Arc
Insight Into Collision Zone Dynamics from Topography: Numerical Modelling Results and Observations
A New Magma Type in the Continental Collision Zone. the Case of Capraia Island (Tuscany, Italy)
Curved Orogenic Belts, Back-Arc Basins, and Obduction As Consequences of Collision at Irregular Continental Margins.', Geology
A Review of Variscan Metamorphism and Deformation in Northern Sardinia
Low-Latitude Arc–Continent Collision As a Driver for Global Cooling
Redalyc.New Active Faults on Eurasian-Arabian Collision Zone: Tectonic Activity of Özyurt and Gülsünler Faults (Eastern Anato
Obduction, Collision Or Deccan-Related Uplift?
Crustal Magnetism, Tectonic Inheritance, and Continental Rifting in the Southeastern United States
GEOFISICA Stress Field and Seismicity at Campi Flegrei Caldera
Subduction to Strike-Slip Transitions on Plate Boundaries
Curved Orogenic Belts, Back-Arc Basins, And
Seismicity and the Long-Term Rheology of Continental Lithosphere: Time to Burn-Out “Crème Brûlée”? Insights from Large-Scale Geodynamic Modeling
Mélanges and Mélange-Forming Processes: a Historical Overview
Seismic-Reflection and Seismic-Refraction Imaging of the South Portuguese Zone Fold-And-Thrust Belt
Top View
GL209 Prof. John Tarney Lecture 3: Wilson Cycle 1 PLATE TECTONICS
The Nature of the Banda Arc–Continent Collision in the Timor Region
Continental Collision and Slab Break-Off: a Comparison of 3-D Numerical Models with Observations
Plate Tectonics
Plate Tectonics and Landform Evolution - D
Slab Rollback Orogeny in the Alps and Evolution of the Swiss Molasse Basin
Future Accreted Terranes: a Compilation of Island Arcs, Oceanic Plateaus, Submarine Ridges, Seamounts, and Continental Fragments
Continental Collision and the Dynamic and Thermal Evolution of the Variscan Orogenic Crustal Root Ð Numerical Models
Accretionary Orogens Through Earth History
Switching Between Alternative Responses of the Lithosphere to Continental Collision
Strike-Slip and Oblique-Slip Tectonics
(Foreland) Basin for Paleoclimatic Research
ARC ASSEMBLY and CONTINENTAL COLLISION in the NEOPROTEROZOIC EAST AFRICAN OROGEN:Implications for the Consolidation of Gondwanaland
The Fate of Subducted Continental Crust: Evidence from Recycled Uhp –Uht Minerals
What Happens When Continents Collide? Crustal Evaluation Education Project
The Case of the Missing Alpine Magmatic
Plates Moving Apart Types of Boundaries PLATE TECTONICS IS the Theory That the Earth’S Crust Is Broken Into Slabs of Rock That Move Around on Top of the Asthenosphere
Collision Vs. Subduction-Related Magmatism: Two Contrasting Ways of Granite Formation and Implications for Crustal Growth Jean-François Moyen, O