All Stories

  1. Weathering pulses during glacial-interglacial transitions: Insights from well-dated paleosols in the Azores volcanic province (Central North Atlantic)
  2. A giant volcanic island in an early Martian Ocean?
  3. Why and how do small volcanic ocean islands collapse? Lessons from Santa Maria Island, Azores
  4. Review of tectonic inversion of sedimentary basins in NE and N Brazil: Analysis of mechanisms, timing and effects on structures and relief
  5. Paleoclimate and weathering on volcanic islands: insights from well-dated paleosols spanning the last Myr in the Central Azores
  6. Multistage evolution of intracontinental basins: the case of the Lusitanian Basin
  7. Influence of hydrothermal silicification on the physical properties of a basin-boundary fault affecting arkosic porous sandstones, Rio do Peixe Basin, Brazil
  8. Relations between inherited basement fabric and fault nucleation in a continental setting: The Rio do Peixe Basin, NE Brazil
  9. Exhumation history of the Variscan orogen in western Iberia as inferred from new K-Ar and 40Ar/39Ar data on granites from Portugal
  10. Thermal evolution of onshore West Iberia: A better understanding of the ages of breakup and rift-to-drift in the Iberia-Newfoundland Rift
  11. The shaping of a volcanic ridge in a tectonically active setting: The Pico-Faial Ridge in the Azores Triple Junction
  12. U–Pb zircon geochronology and phase equilibria modelling of HP-LT rocks in the Ossa-Morena Zone, Portugal
  13. Tectonic inversion assessed by integration of geological and geophysical data: The intracontinental Rio do Peixe Basin, NE Brazil
  14. Volcanic Record of the Last Geomagnetic Reversal in a Lava Flow Sequence From the Azores
  15. The evolution of Santa Maria Island in the context of the Azores Triple Junction
  16. The Complex Vertical Motion of Intraplate Oceanic Islands Assessed in Santiago Island, Cape Verde
  17. Caldera or flank collapse in the Fogo volcano? What age? Consequences for risk assessment in volcanic islands
  18. Basin development by relaxation of a buckled elastic layer: Insights from laboratory experiments
  19. Comment on Lithospheric and sub-lithospheric deformation under the Borborema Province of NE Brazil from receiver function harmonic stripping
  20. Corrigendum to “Tectonic overpressure at shallow depth in the lithosphere: The effects of boundary conditions” [Tectonophysics 746 (2018) 702–715]
  21. Reply to Platt's comment
  22. Tectonic overpressure at shallow depth in the lithosphere: The effects of boundary conditions
  23. Large-scale mass wasting on small volcanic islands revealed by the study of Flores Island (Azores)
  24. Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas
  25. Response to Reviewer#2's comments
  26. Evolution of a volcanic island on the shoulder of an oceanic rift and geodynamic implications: S. Jorge Island on the Terceira Rift, Azores Triple Junction
  27. Response to Reviewer#2's comments
  28. Response to Reviewer#1's comments
  29. Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas
  30. Volcano-tectonic evolution of a linear volcanic ridge (Pico-Faial Ridge, Azores Triple Junction) assessed by paleomagnetic studies
  31. Sentinel-1 InSAR data applied to surface deformation in Macaronesia (Canaries and Cape Verde)
  32. Mineral lineation produced by 3-D rotation of rigid inclusions in confined viscous simple shear
  33. Structural consequences of cohesion in gravitational instabilities triggered by fluid overpressure: Analytical derivation and experimental testing
  34. Insular shelves
  35. Post-buckling relaxation of an elastic layer and its geological relevance: Insights from analogue experiments in pure shear
  36. Deformation in a hyperslow oceanic rift: Insights from the tectonics of the São Miguel Island (Terceira Rift, Azores)
  37. Speculations on the impact of catastrophic subduction initiation on the Earth System
  38. Catastrophic flank collapses and slumping in Pico Island during the last 130 kyr (Pico-Faial ridge, Azores Triple Junction)
  39. Reply to the comment by Quartau et al. on “Construction and destruction of a volcanic island developed inside an oceanic rift: Graciosa Island, Terceira Rift, Azores”, J. Volcanol. Geotherm. Res. 284, 32–45, by Sibrant et al. (2014)
  40. Mechanics, microstructure and AMS evolution of a synthetic porphyritic calcite aggregate deformed in torsion
  41. Morpho-structural evolution of a volcanic island developed inside an active oceanic rift: S. Miguel Island (Terceira Rift, Azores)
  42. Ground motion and tectonics in the Terceira Island: Tectonomagmatic interactions in an oceanic rift (Terceira Rift, Azores Triple Junction)
  43. Cretaceous intracontinental rifting and post-rift inversion in NE Brazil: Insights from the Rio do Peixe Basin
  44. Volcano-tectonic evolution of the Santa Maria Island (Azores): Implications for paleostress evolution at the western Eurasia–Nubia plate boundary
  45. Recent plate re-organization at the Azores Triple Junction: Evidence from combined geochemical and geochronological data on Faial, S. Jorge and Terceira volcanic islands
  46. The 1998 Faial earthquake, Azores: Evidence for a transform fault associated with the Nubia–Eurasia plate boundary?
  47. Construction and destruction of a volcanic island developed inside an oceanic rift: Graciosa Island, Terceira Rift, Azores
  48. The Araripe Basin in NE Brazil: An intracontinental graben inverted to a high-standing horst
  49. Evidence for non-coaxiality of ferrimagnetic and paramagnetic fabrics, developed during magma flow and cooling in a thick mafic dyke
  50. Intrusion of lamprophyre dyke and related deformation effects in the host rock salt: A case study from the Loulé diapir, Portugal
  51. The behaviour of deformable and non-deformable inclusions in viscous flow
  52. Subduction initiates at straight passive margins
  53. Are subduction zones invading the Atlantic? Evidence from the southwest Iberia margin: COMMENT
  54. Corrigendum to “GPS and tectonic evidence for a diffuse plate boundary at the Azores Triple Junction” [Earth Planet. Sci. Lett. 381 (2013) 177–187]
  55. Large-scale catastrophic flank collapses in a steep volcanic ridge: The Pico–Faial Ridge, Azores Triple Junction
  56. Is the ‘Azores Hotspot’ a Wetspot? Insights from the Geochemistry of Fluid and Melt Inclusions in Olivine of Pico Basalts
  57. Large-scale active slump of the southeastern flank of Pico Island, Azores: REPLY
  58. GPS and tectonic evidence for a diffuse plate boundary at the Azores Triple Junction
  59. Testing the influence of far-field topographic forcing on subduction initiation at a passive margin
  60. Palaeomagnetism in the Sines massif (SW Iberia) revisited: evidences for Late Cretaceous hydrothermal alteration and associated partial remagnetization
  61. Reply to the comment by Quartau and Mitchell on “Reconstructing the architectural evolution of volcanic islands from combined K/Ar, morphologic, tectonic, and magnetic data: The Faial Island example (Azores)”, J. Volcanol. Geotherm. Res. 241–242, 39–48...
  62. Cenozoic uplift and erosion of structural landforms in NE Brazil
  63. Rheology of synthetic polycrystalline halite in torsion
  64. Large-scale active slump of the southeastern flank of Pico Island, Azores
  65. Reconstructing the architectural evolution of volcanic islands from combined K/Ar, morphologic, tectonic, and magnetic data: The Faial Island example (Azores)
  66. Comment on “Eye and sheath folds in turbidite convolute lamination: Aberystwyth Grits Group, Wales”, by H.L.O. McClelland, N.H. Woodcock, C. Gladstone, Journal of Structural Geology 33 (2011) 1140–1147
  67. Boudinage in nature and experiment
  68. Modelling in geosciences
  69. Transform faults orthogonal to rifts: Insights from fully gravitational physical experiments
  70. Palaeomagnetic study of a subaerial volcanic ridge (São Jorge Island, Azores) for the past 1.3 Myr: evidence for the Cobb Mountain Subchron, volcano flank instability and tectonomagmatic implications
  71. Microstructural and mechanical effects of strong fine-grained muscovite in soft halite matrix: Shear strain localization in torsion
  72. Numerical analysis of subduction initiation risk along the Atlantic American passive margins
  73. Microstructure and mechanical properties of halite/coarse muscovite synthetic aggregates deformed in torsion
  74. Thick dyke emplacement and internal flow: A structural and magnetic fabric study of the deep-seated dolerite dyke of Foum Zguid (southern Morocco)
  75. Dynamic unfolding of multilayers: 2D numerical approach and application to turbidites in SW Portugal
  76. Technical note on the strength of copper versus polymer jackets in torsion tests on halite up to 300°C
  77. Comment on “Deep structure, recent deformation and analog modeling of the Gulf of Cadiz accretionary wedge: Implications for the 1755 Lisbon earthquake”, by Gutscher et al. 2009
  78. Fluid-assisted particulate flow of turbidites at very low temperature: A key to tight folding in a submarine Variscan foreland basin of SW Europe
  79. Subduction initiation at passive margins: Numerical modeling
  80. Rheology and microstructure of synthetic halite/calcite porphyritic aggregates in torsion
  81. Reply to discussion by G.I. Alsop and R.E. Holdsworth of “Sheath fold development with viscosity contrast: analogue experiments in bulk simple shear” by Marques et al., Journal of Structural Geology, 30, 1348–1353.
  82. A thin elastic core can control large-scale patterns of lithosphere shortening
  83. Initial stages of pollutants dispersion around municipal waste disposal facilities: a case study in Northern Portugal
  84. Geodynamic evolution of the SW Variscides: Orogenic collapse shown by new tectonometamorphic and isotopic data from western Ossa-Morena Zone, SW Iberia
  85. Sheath fold development with viscosity contrast: Analogue experiments in bulk simple shear
  86. Magma flow, exsolution processes and rock metasomatism in the Great Messejana-Plasencia dyke (Iberian Peninsula)
  87. Rigid inclusions rotate in geologic materials as shown by torsion experiments
  88. Multi-stage evolution of a sub-aerial volcanic ridge over the last 1.3 Myr: S. Jorge Island, Azores Triple Junction
  89. Normal fault inversion by orthogonal compression: Sandbox experiments with weak faults
  90. Thrust initiation and propagation during shortening of a 2-layer model lithosphere
  91. Applications of inclusion behaviour models to a major shear zone system: The Nordfjord-Sogn Detachment Zone in western Norway
  92. Physical models of rifting and transform faulting, due to ridge push in a wedge-shaped oceanic lithosphere
  93. Paleomagnetic study of the Great Foum Zguid dyke (southern Morocco): A positive contact test related to metasomatic processes
  94. Riedel-shear control on the development of pennant veins: Field example and analogue modelling
  95. Comment on “Numerical models of flow patterns around a rigid inclusion in a viscous matrix undergoing simple shear: implications of model parameters and boundary conditions” by N. Mandal, S.K. Samanta and C. Chakraborty [Journal of Structural Geology 2...
  96. Effects of topography on the curvature of fold-and-thrust belts during shortening of a 2-layer model of continental lithosphere
  97. Variation of magnetic properties in sedimentary rocks hosting the Foum Zguid dyke (southern Morocco): Combined effects of re-crystallization and Fe-metasomatism
  98. Influence of a low-viscosity layer between rigid inclusion and viscous matrix on inclusion rotation and matrix flow: A numerical study
  99. The effectiveness of “clay” liners as basal isolation of landfills: a case study
  100. Effects of confinement on matrix flow around a rigid inclusion in viscous simple shear: insights from analogue and numerical modelling
  101. 2D rotation of rigid inclusions in confined bulk simple shear flow: a numerical study
  102. Controls on the geometry of tails around rigid circular inclusions: insights from analogue modelling in simple shear
  103. Granite fracturing and incipient pollution beneath a recent landfill facility as detected by geoelectrical surveys
  104. Influence of a permanent low-friction boundary on rotation and flow in rigid inclusion/viscous matrix systems from an analogue perspective
  105. 2-D rotation behavior of a rigid ellipse in confined viscous simple shear: numerical experiments using FEM
  106. Preliminary results of a study of magnetic properties in the Foum-Zguid dyke (Morocco)
  107. 2-D shape preferred orientations of rigid particles in transtensional viscous flow
  108. The Late-Variscan fault network in central–northern Portugal (NW Iberia): a re-evaluation
  109. Reconstruction/Interpretation of Macroscopic Structures from Discontinuous Mesoscopic Observations: a Major Task of Field/Structural Geologists
  110. Topography as a major factor in the development of arcuate thrust belts: insights from sandbox experiments
  111. Sheath folds formed by drag induced by rotation of rigid inclusions in viscous simple shear flow: nature and experiment
  112. New analytical and numerical geospeedometers tested on garnet pyroxenites from Bragança Nappe Complex (NE Portugal)
  113. Anisotropy of magnetic susceptibility constraints on Variscan obduction processes in the Bragança Massif (NE Portugal)
  114. Rotation of rigid elliptical cylinders in viscous simple shear flow: analogue experiments
  115. Flow and fracturing of clay: Analogue experiments in bulk pure shear
  116. Sheath fold development in bulk simple shear: Analogue modeling of natural examples from the Southern Iberian Variscan fold belt
  117. Plastic deformation of silicate garnets
  118. Geodynamic evolution of the Continental Allochthonous Terrane (CAT) of the Bragança Nappe Complex, NE Portugal
  119. Development of highly non-cylindrical folds around rigid ellipsoidal inclusions in bulk simple shear regimes: natural examples and experimental modelling
  120. Discussion
  121. Tectonic evolution of the deep crust: Variscan reactivation by extension and thrusting of Precambrian basement in the Bragança and Morais massifs (Tras-os-Montes, NE Portugal)
  122. Polyphase Variscan emplacement of exotic terranes (Morais and Bragança Massifs) onto Iberian successions: Evidence from 40Ar/39Ar mineral ages