All Stories

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