All Stories

  1. Mapping global kimberlite potential from reconstructions of mantle flow over the past billion years
  2. The deep roots of Earth’s surface
  3. Quantitative stratigraphic analysis in a source-to-sink numerical framework
  4. Constraining absolute plate motions since the Triassic
  5. The interplay of dynamic topography and eustasy on continental flooding in the late Paleozoic
  6. Erratum: Present-dayd dynamic topography and lower mantle structure from paleogeographically-constrained mantle flow models
  7. Present-day dynamic topography and lower mantle structure from paleogeographically-constrained mantle flow models
  8. Quantitative stratigraphic analysis in a source-to-sink numerical framework
  9. Quantitative stratigraphic analysis in a source-to-sink numerical framework
  10. Geodynamic reconstruction of an accreted Cretaceous back-arc basin in the Northern Andes
  11. On the scales of dynamic topography in whole-mantle convection models
  12. Global kinematics of tectonic plates and subduction zones since the late Paleozoic Era
  13. The Dynamic Topography of Eastern China Since the Latest Jurassic Period
  14. Global tectonic reconstructions with continuously deforming and evolving rigid plates
  15. Palaeolatitudinal distribution of lithologic indicators of climate in a palaeogeographic framework
  16. Dynamic topography of passive continental margins and their hinterlands since the Cretaceous
  17. Improving global paleogeography since the late Paleozoic using paleobiology
  18. The role of deep Earth dynamics in driving the flooding and emergence of New Guinea since the Jurassic
  19. Correspondence: Reply to ‘Numerical modelling of the PERM anomaly and the Emeishan large igneous province’
  20. Dynamic topography and eustasy controlled the paleogeographic evolution of northern Africa since the mid-Cretaceous
  21. Improving global paleogeography since the late Paleozoic using paleobiology
  22. Improving global paleogeography since the late Paleozoic using paleobiology
  23. The deep Earth origin of the Iceland plume and its effects on regional surface uplift and subsidence
  24. Origin and evolution of the deep thermochemical structure beneath Eurasia
  25. Influence of mantle flow on the drainage of eastern Australia since the Jurassic Period
  26. Tectonic evolution and deep mantle structure of the eastern Tethys since the latest Jurassic
  27. Large fluctuations of shallow seas in low-lying Southeast Asia driven by mantle flow
  28. A rapid burst in hotspot motion through the interaction of tectonics and deep mantle flow
  29. Formation of Australian continental margin highlands driven by plate–mantle interaction
  30. The GPlates Portal: Cloud-Based Interactive 3D Visualization of Global Geophysical and Geological Data in a Web Browser
  31. Alignment between seafloor spreading directions and absolute plate motions through time
  32. Influence of subduction history on South American topography
  33. Tectonic speed limits from plate kinematic reconstructions
  34. Absolute plate motions since 130 Ma constrained by subduction zone kinematics
  35. Provenance of plumes in global convection models
  36. Ridge subduction sparked reorganization of the Pacific plate-mantle system 60-50 million years ago
  37. Assimilating lithosphere and slab history in 4-D Earth models
  38. Circum-Arctic mantle structure and long-wavelength topography since the Jurassic
  39. Linking plate tectonics and mantle flow to Earth's topography
  40. Spreading continents kick-started plate tectonics
  41. Cenozoic uplift of south Western Australia as constrained by river profiles
  42. Topographic asymmetry of the South Atlantic from global models of mantle flow and lithospheric stretching
  43. The evolution of the 87Sr/86Sr of marine carbonates does not constrain continental growth
  44. A review of observations and models of dynamic topography
  45. A deep subaqueous fan depositional model for the Palaeoarchaean (3.46 Ga) Marble Bar Cherts, Warrawoona Group, Western Australia
  46. Insights on the kinematics of the India-Eurasia collision from global geodynamic models
  47. Lower crustal flow kept Archean continental flood basalts at sea level
  48. A case for late-Archaean continental emergence from thermal evolution models and hypsometry