All Stories

  1. Influence of tectonic regime superposition on damage zone structures in a basin-boundary fault, Jatobá basin, NE Brazil
  2. Restoring volcanic ocean island palaeotopography to uncover island-scale buried sector collapses
  3. Experimental Modeling of En Masse Translation of Long Brittle Blocks Over a Viscous Layer: Application to the Sichuan Basin, China
  4. Fast CO2 uptake by intense weathering of volcanic islands during interglacial stages
  5. Dynamics and evolution of the Azores Triple Junction and its relation to pre-existing major tectonic structures
  6. Effects of backstop vertical position on the evolution of a backthrust dominated fold-and-thrust belt: Insights from viscous/brittle analogue models and comparison with cascadia
  7. How and why small volcanic ocean islands collapse and move vertically up and down
  8. Tectonic Inversion of Intracontinental Basins and the Conundrum of Plate‐Scale Stress Propagation: The Case of the Jatobá Basin, NE Brazil
  9. Precise dating of large flank collapses by single-grain 40Ar/39Ar on pyroclastic deposits from the example of Flores Island (Azores)
  10. Regional Variations of the Azores High Across Glacial‐Interglacial Timescales
  11. Weathering pulses during glacial-interglacial transitions: Insights from well-dated paleosols in the Azores volcanic province (Central North Atlantic)
  12. A giant volcanic island in an early Martian Ocean?
  13. Review of tectonic inversion of sedimentary basins in NE and N Brazil: Analysis of mechanisms, timing and effects on structures and relief
  14. Influence of hydrothermal silicification on the physical properties of a basin-boundary fault affecting arkosic porous sandstones, Rio do Peixe Basin, Brazil
  15. Relations between inherited basement fabric and fault nucleation in a continental setting: The Rio do Peixe Basin, NE Brazil
  16. Exhumation history of the Variscan orogen in western Iberia as inferred from new K-Ar and 40Ar/39Ar data on granites from Portugal
  17. Thermal evolution of onshore West Iberia: A better understanding of the ages of breakup and rift-to-drift in the Iberia-Newfoundland Rift
  18. The shaping of a volcanic ridge in a tectonically active setting: The Pico-Faial Ridge in the Azores Triple Junction
  19. U–Pb zircon geochronology and phase equilibria modelling of HP-LT rocks in the Ossa-Morena Zone, Portugal
  20. Tectonic inversion assessed by integration of geological and geophysical data: The intracontinental Rio do Peixe Basin, NE Brazil
  21. Volcanic Record of the Last Geomagnetic Reversal in a Lava Flow Sequence From the Azores
  22. The evolution of Santa Maria Island in the context of the Azores Triple Junction
  23. The Complex Vertical Motion of Intraplate Oceanic Islands Assessed in Santiago Island, Cape Verde
  24. Caldera or flank collapse in the Fogo volcano? What age? Consequences for risk assessment in volcanic islands
  25. Basin development by relaxation of a buckled elastic layer: Insights from laboratory experiments
  26. Comment on Lithospheric and sub-lithospheric deformation under the Borborema Province of NE Brazil from receiver function harmonic stripping
  27. Corrigendum to “Tectonic overpressure at shallow depth in the lithosphere: The effects of boundary conditions” [Tectonophysics 746 (2018) 702–715]
  28. Reply to Platt's comment
  29. Tectonic overpressure at shallow depth in the lithosphere: The effects of boundary conditions
  30. Large-scale mass wasting on small volcanic islands revealed by the study of Flores Island (Azores)
  31. Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas
  32. Response to Reviewer#2's comments
  33. 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
  34. Response to Reviewer#2's comments
  35. Response to Reviewer#1's comments
  36. Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas
  37. Volcano-tectonic evolution of a linear volcanic ridge (Pico-Faial Ridge, Azores Triple Junction) assessed by paleomagnetic studies
  38. Sentinel-1 InSAR data applied to surface deformation in Macaronesia (Canaries and Cape Verde)
  39. Mineral lineation produced by 3-D rotation of rigid inclusions in confined viscous simple shear
  40. Structural consequences of cohesion in gravitational instabilities triggered by fluid overpressure: Analytical derivation and experimental testing
  41. Insular shelves
  42. Post-buckling relaxation of an elastic layer and its geological relevance: Insights from analogue experiments in pure shear
  43. Deformation in a hyperslow oceanic rift: Insights from the tectonics of the São Miguel Island (Terceira Rift, Azores)
  44. Speculations on the impact of catastrophic subduction initiation on the Earth System
  45. Catastrophic flank collapses and slumping in Pico Island during the last 130 kyr (Pico-Faial ridge, Azores Triple Junction)
  46. 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)
  47. Mechanics, microstructure and AMS evolution of a synthetic porphyritic calcite aggregate deformed in torsion
  48. Morpho-structural evolution of a volcanic island developed inside an active oceanic rift: S. Miguel Island (Terceira Rift, Azores)
  49. Ground motion and tectonics in the Terceira Island: Tectonomagmatic interactions in an oceanic rift (Terceira Rift, Azores Triple Junction)
  50. Cretaceous intracontinental rifting and post-rift inversion in NE Brazil: Insights from the Rio do Peixe Basin
  51. Volcano-tectonic evolution of the Santa Maria Island (Azores): Implications for paleostress evolution at the western Eurasia–Nubia plate boundary
  52. Recent plate re-organization at the Azores Triple Junction: Evidence from combined geochemical and geochronological data on Faial, S. Jorge and Terceira volcanic islands
  53. The 1998 Faial earthquake, Azores: Evidence for a transform fault associated with the Nubia–Eurasia plate boundary?
  54. Construction and destruction of a volcanic island developed inside an oceanic rift: Graciosa Island, Terceira Rift, Azores
  55. The Araripe Basin in NE Brazil: An intracontinental graben inverted to a high-standing horst
  56. Evidence for non-coaxiality of ferrimagnetic and paramagnetic fabrics, developed during magma flow and cooling in a thick mafic dyke
  57. Intrusion of lamprophyre dyke and related deformation effects in the host rock salt: A case study from the Loulé diapir, Portugal
  58. The behaviour of deformable and non-deformable inclusions in viscous flow
  59. Subduction initiates at straight passive margins
  60. Are subduction zones invading the Atlantic? Evidence from the southwest Iberia margin: COMMENT
  61. Corrigendum to “GPS and tectonic evidence for a diffuse plate boundary at the Azores Triple Junction” [Earth Planet. Sci. Lett. 381 (2013) 177–187]
  62. Large-scale catastrophic flank collapses in a steep volcanic ridge: The Pico–Faial Ridge, Azores Triple Junction
  63. Is the ‘Azores Hotspot’ a Wetspot? Insights from the Geochemistry of Fluid and Melt Inclusions in Olivine of Pico Basalts
  64. Large-scale active slump of the southeastern flank of Pico Island, Azores: REPLY
  65. GPS and tectonic evidence for a diffuse plate boundary at the Azores Triple Junction
  66. Testing the influence of far-field topographic forcing on subduction initiation at a passive margin
  67. Palaeomagnetism in the Sines massif (SW Iberia) revisited: evidences for Late Cretaceous hydrothermal alteration and associated partial remagnetization
  68. 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...
  69. Cenozoic uplift and erosion of structural landforms in NE Brazil
  70. Rheology of synthetic polycrystalline halite in torsion
  71. Large-scale active slump of the southeastern flank of Pico Island, Azores
  72. Reconstructing the architectural evolution of volcanic islands from combined K/Ar, morphologic, tectonic, and magnetic data: The Faial Island example (Azores)
  73. 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
  74. Boudinage in nature and experiment
  75. Modelling in geosciences
  76. Transform faults orthogonal to rifts: Insights from fully gravitational physical experiments
  77. 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
  78. Microstructural and mechanical effects of strong fine-grained muscovite in soft halite matrix: Shear strain localization in torsion
  79. Numerical analysis of subduction initiation risk along the Atlantic American passive margins
  80. Microstructure and mechanical properties of halite/coarse muscovite synthetic aggregates deformed in torsion
  81. Thick dyke emplacement and internal flow: A structural and magnetic fabric study of the deep-seated dolerite dyke of Foum Zguid (southern Morocco)
  82. Dynamic unfolding of multilayers: 2D numerical approach and application to turbidites in SW Portugal
  83. Technical note on the strength of copper versus polymer jackets in torsion tests on halite up to 300°C
  84. 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
  85. Fluid-assisted particulate flow of turbidites at very low temperature: A key to tight folding in a submarine Variscan foreland basin of SW Europe
  86. Subduction initiation at passive margins: Numerical modeling
  87. Rheology and microstructure of synthetic halite/calcite porphyritic aggregates in torsion
  88. 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.
  89. A thin elastic core can control large-scale patterns of lithosphere shortening
  90. Initial stages of pollutants dispersion around municipal waste disposal facilities: a case study in Northern Portugal
  91. Geodynamic evolution of the SW Variscides: Orogenic collapse shown by new tectonometamorphic and isotopic data from western Ossa-Morena Zone, SW Iberia
  92. Sheath fold development with viscosity contrast: Analogue experiments in bulk simple shear
  93. Magma flow, exsolution processes and rock metasomatism in the Great Messejana-Plasencia dyke (Iberian Peninsula)
  94. Rigid inclusions rotate in geologic materials as shown by torsion experiments
  95. Multi-stage evolution of a sub-aerial volcanic ridge over the last 1.3 Myr: S. Jorge Island, Azores Triple Junction
  96. Normal fault inversion by orthogonal compression: Sandbox experiments with weak faults
  97. Thrust initiation and propagation during shortening of a 2-layer model lithosphere
  98. Applications of inclusion behaviour models to a major shear zone system: The Nordfjord-Sogn Detachment Zone in western Norway
  99. Physical models of rifting and transform faulting, due to ridge push in a wedge-shaped oceanic lithosphere
  100. Paleomagnetic study of the Great Foum Zguid dyke (southern Morocco): A positive contact test related to metasomatic processes
  101. Riedel-shear control on the development of pennant veins: Field example and analogue modelling
  102. 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...
  103. Effects of topography on the curvature of fold-and-thrust belts during shortening of a 2-layer model of continental lithosphere
  104. Variation of magnetic properties in sedimentary rocks hosting the Foum Zguid dyke (southern Morocco): Combined effects of re-crystallization and Fe-metasomatism
  105. Influence of a low-viscosity layer between rigid inclusion and viscous matrix on inclusion rotation and matrix flow: A numerical study
  106. The effectiveness of “clay” liners as basal isolation of landfills: a case study
  107. Effects of confinement on matrix flow around a rigid inclusion in viscous simple shear: insights from analogue and numerical modelling
  108. 2D rotation of rigid inclusions in confined bulk simple shear flow: a numerical study
  109. Controls on the geometry of tails around rigid circular inclusions: insights from analogue modelling in simple shear
  110. Granite fracturing and incipient pollution beneath a recent landfill facility as detected by geoelectrical surveys
  111. Influence of a permanent low-friction boundary on rotation and flow in rigid inclusion/viscous matrix systems from an analogue perspective
  112. 2-D rotation behavior of a rigid ellipse in confined viscous simple shear: numerical experiments using FEM
  113. Preliminary results of a study of magnetic properties in the Foum-Zguid dyke (Morocco)
  114. 2-D shape preferred orientations of rigid particles in transtensional viscous flow
  115. The Late-Variscan fault network in central–northern Portugal (NW Iberia): a re-evaluation
  116. Reconstruction/Interpretation of Macroscopic Structures from Discontinuous Mesoscopic Observations: a Major Task of Field/Structural Geologists
  117. Topography as a major factor in the development of arcuate thrust belts: insights from sandbox experiments
  118. Sheath folds formed by drag induced by rotation of rigid inclusions in viscous simple shear flow: nature and experiment
  119. New analytical and numerical geospeedometers tested on garnet pyroxenites from Bragança Nappe Complex (NE Portugal)
  120. Anisotropy of magnetic susceptibility constraints on Variscan obduction processes in the Bragança Massif (NE Portugal)
  121. Rotation of rigid elliptical cylinders in viscous simple shear flow: analogue experiments
  122. Flow and fracturing of clay: Analogue experiments in bulk pure shear
  123. Sheath fold development in bulk simple shear: Analogue modeling of natural examples from the Southern Iberian Variscan fold belt
  124. Plastic deformation of silicate garnets
  125. Geodynamic evolution of the Continental Allochthonous Terrane (CAT) of the Bragança Nappe Complex, NE Portugal
  126. Development of highly non-cylindrical folds around rigid ellipsoidal inclusions in bulk simple shear regimes: natural examples and experimental modelling
  127. Discussion
  128. 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)
  129. Polyphase Variscan emplacement of exotic terranes (Morais and Bragança Massifs) onto Iberian successions: Evidence from 40Ar/39Ar mineral ages