All Stories

  1. Exploring Rift Tectonovolcanism in Venus
  2. Influence of lower crustal rheology on orogenic growth modes
  3. Mapping Tectonic Lineaments in Venus
  4. New mapping and geochronology constraints on the Variscan plutonism, metamorphism and deformation in the Ossa-Morena Zone (SW Iberian Massif)
  5. Subduction invasion of the Atlantic
  6. 2D thermomechanical numerical models of passive margin reactivation
  7. 3D Numerical modelling of induced subduction initiation by transference
  8. Exo-Geoscience Perspectives Beyond Habitability
  9. Geodynamics of forearc topography and strain linked with giant earthquake rupture area
  10. Tectonic plate delamination could explain large earthquakes at the Iberian Margin
  11. Experimental Modeling of En Masse Translation of Long Brittle Blocks Over a Viscous Layer: Application to the Sichuan Basin, China
  12. Volcanic gas plumes’ effect on the spectrum of Venus
  13. Seismic evidence for oceanic plate delamination offshore Southwest Iberia
  14. Numerical Geodynamic Modeling of Buoyancy‐Driven Tethyan‐type Ophiolite Emplacement
  15. VOLCANIC GAS PLUMES’ EFFECTS ON THE SPECTRUM OF VENUS – THE 1.18 µM WINDOW
  16. Subduction transference drove the Mesozoic convergence of microcontinents from Gondwana to Asia
  17. Ocean circulation on a temperate paleo-Venus simulated with ROCKE-3D
  18. Variscan plutonism in the Ossa-Morena Zone (SW Iberian Massif): The Mississippian and Pennsylvanian magmatism and its importance for the regional tectonic sequence of events
  19. 2D Numerical modelling of continental subduction and synthetic obduction
  20. 2D numerical models of passive margin reactivation
  21. Analogue modeling of strike-slip faults: a new insight from different kinematic constrains
  22. Evidence for onset of convergent tectonics within the Continent-Ocean Transition zones of the Atlantic rifted margins
  23. Evidence of oceanic plate delamination in the Northern Atlantic
  24. Modes of collisional orogenic growth: forward, backward and thermally induced
  25. The effect of oceanic forearc serpentinization on ophiolite emplacement: Insights from 3D geodynamic models
  26. Tracking a common mantle plume, from Iberia to Canarias-Madeira
  27. Insights into plume-ridge-transform fault interactions as derived from 3D numerical geodynamic modelling of the Azores Triple Junction
  28. Tracking a common mantle source: From southwest Iberia to the Madeira-Canarias Islands
  29. The European Fault-Source Model 2020 (EFSM20): geologic input data for the European Seismic Hazard Model 2020
  30. A new geodynamic model of the Azores archipelago: preliminary results
  31. Gibraltar subduction zone is invading the Atlantic
  32. Proto-ophiolite serpentinization may influence ophiolite emplacement: Insights from numerical models 
  33. Gibraltar subduction zone is invading the Atlantic
  34. Supplemental Material: Gibraltar subduction zone is invading the Atlantic
  35. Supplemental Material: Gibraltar subduction zone is invading the Atlantic
  36. The European Fault-Source Model 2020 (EFSM20): geologic input data for the European Seismic Hazard Model 2020
  37. 2D numerical modelling of Tethyan-type ophiolite emplacement: The role of overriding plate age, serpentinization, and OCT width.
  38. Alpine subduction and intraplate deformation along the Iberian Atlantic margins
  39. Geodynamic modelling of continental subduction beneath oceanic lithosphere
  40. How do subduction zones spread over Atlantic-type oceans?
  41. Numerical modelling of intra-oceanic rifting: the rift-to-drift transition time frame
  42. Resolving Late Cretaceous intra-plate magmatism emplacement models and plate motion on the West Iberian Margin
  43. Subduction invasion polarity switch (SIPS):  A new mechanism of subduction initiation, with an application to the Scotia Sea region
  44. Subduction initiation triggered the Caribbean large igneous province
  45. Sunda subduction drives ongoing India-Asia convergence
  46. Subduction invasion polarity switch from the Pacific to the Atlantic Ocean: A new geodynamic model of subduction initiation based on the Scotia Sea region
  47. A Journey Through Tides
  48. Dynamics of Plate Tectonics and Mantle Convection
  49. Impact of crustal rheology and inherited mechanical weaknesses on early continental rifting and initial evolution of double graben structural configurations: Insights from 2D numerical models
  50. Numerical modeling of subduction zones: thermo-mechanical stabilization as a function of overriding plate rheology and thickness
  51. Subduction invasion of the Atlantic by Mediterranean subduction zones
  52. Tides And Relative Dissipation In Supercycles – An overview of tidal modelling work with OTIS and what’s next.
  53. Self-replicating subduction zone initiation by polarity reversal
  54. Self-replicating subduction zone initiation by polarity reversal
  55. Polarity-reversal subduction zone initiation triggered by buoyant plateau obstruction
  56. Evidence of oceanic plate delamination in the Northern Atlantic
  57. Evolution of parallel, oblique and triple-junction rifts: Insights from analogue modelling
  58. The Climates of Earth’s Next Supercontinent: Effects of Tectonics, Rotation Rate, and Insolation
  59. The climates of Earth's next supercontinent: effects of tectonics, rotation rate, and insolation
  60. Analysing the tidal state of a pre-plate tectonic Earth during the Archean Eon (3.9 Ga)
  61. Tides on a Snowball
  62. Weak tides during Cryogenian glaciations
  63. Dynamics of the Gibraltar Arc System: A complex interaction between plate convergence, slab pull and mantle flow
  64. Back to the future II: tidal evolution of four supercontinent scenarios
  65. Back to the future 3: Analysing tectonically induced tidal resonance with conceptual models
  66. Quest for Fluid Flow along the Gloria Fault – First results of R/V Meteor expedition 162
  67. The climates of Earth's next supercontinent: effects of tectonics, rotation rate, and insolation
  68. Deep Future Climate on Earth: effects of tectonics, rotation rate, and insolation
  69. Back to the Future II: Tidal evolution of four supercontinent scenarios
  70. Back to the Future II: Tidal evolution of four supercontinent scenarios
  71. Pacific subduction control on Asian continental deformation including Tibetan extension and eastward extrusion tectonics
  72. Analogue modelling of brittle shear zone propagation across upper crustal morpho-rheological heterogeneities
  73. Reativação tectónica
  74. Marine Transform Faults and Fracture Zones: A Joint Perspective Integrating Seismicity, Fluid Flow and Life
  75. The Alpine Orogeny in the West and Southwest Iberia Margins
  76. What will the next Supercontinent look like?
  77. Is There a Tectonically Driven Supertidal Cycle?
  78. Topography of the Overriding Plate During Progressive Subduction: A Dynamic Model to Explain Forearc Subsidence
  79. Micro-seismicity in the Gulf of Cadiz: Is there a link between micro-seismicity, high magnitude earthquakes and active faults?
  80. Analogue modelling of thrust systems: Passive vs. active hanging wall strain accommodation and sharp vs. smooth fault-ramp geometries
  81. Recent uplift of the Atlantic Atlas (offshore West Morocco): Tectonic arch and submarine terraces
  82. Plate Boundaries and Natural Hazards
  83. Mantle plumes in the vicinity of subduction zones
  84. Introduction to Plate Boundaries and Natural Hazards
  85. Seismic Potential of Thrust-Wrench Tectonic Interference between Major Active Faults Offshore SW Iberia
  86. The future of Earth's oceans: consequences of subduction initiation in the Atlantic and implications for supercontinent formation
  87. Lithospheric deformation in the Africa-Iberia plate boundary: Improved neotectonic modeling testing a basal-driven Alboran plate
  88. Plate Boundaries and Natural Hazards
  89. Does subduction-induced mantle flow drive backarc extension?
  90. The variation of crustal stretching and different modes of rifting along the Australian southern continental margin
  91. Overriding plate deformation and variability of fore-arc deformation during subduction: Insight from geodynamic models and application to the Calabria subduction zone
  92. A two-way interaction between the Hainan plume and the Manila subduction zone
  93. Geodynamic models of continental subduction and obduction of overriding plate forearc oceanic lithosphere on top of continental crust
  94. Analogue modelling of different angle thrust-wrench fault interference in a brittle medium
  95. How weak is the subduction zone interface?
  96. Capture of the Canary mantle plume material by the Gibraltar arc mantle wedge during slab rollback
  97. Quantifying the energy dissipation of overriding plate deformation in three-dimensional subduction models
  98. Rheology of petrolatum–paraffin oil mixtures: Applications to analogue modelling of geological processes
  99. Are subduction zones invading the Atlantic? Evidence from the southwest Iberia margin: REPLY
  100. Are subduction zones invading the Atlantic? Evidence from the southwest Iberia margin
  101. Three-dimensional dynamic laboratory models of subduction with an overriding plate and variable interplate rheology
  102. The Gibraltar subduction: A decade of new geophysical data
  103. Thrust–wrench interference between major active faults in the Gulf of Cadiz (Africa–Eurasia plate boundary, offshore SW Iberia): Tectonic implications from coupled analog and numerical modeling
  104. Thrust–wrench interference tectonics in the Gulf of Cadiz (Africa–Iberia plate boundary in the North-East Atlantic): Insights from analog models
  105. Crescent-shaped morphotectonic features in the Gulf of Cadiz (offshore SW Iberia)
  106. Morphotectonics and strain partitioning at the Iberia–Africa plate boundary from multibeam and seismic reflection data
  107. Morphotectonic characterization of major bathymetric lineaments in Gulf of Cadiz (Africa–Iberia plate boundary): Insights from analogue modelling experiments