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Imaging, mapping and modelling continental lithosphere extension and breakup: an introduction |
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1 | (8) |
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The Iberia-Newfoundland continental extensional system (geological and geophysical constraints) |
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Breakup of the Newfoundland-Iberia rift |
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9 | (38) |
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Structure of the Flemish Cap margin, Newfoundland: insights into mantle and crustal processes during continental breakup |
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47 | (16) |
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Early Cretaceous motion of Flemish Cap with respect to North America: implications on the formation of Orphan Basin and SE Flemish Cap-Galicia Bank conjugate margins |
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63 | (14) |
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The formation of non-volcanic rifted margins by the progressive extension of the lithosphere: the example of the West Iberian margin |
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77 | (34) |
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The Iberia-Newfoundland continental extensional system (dynamic modelling) |
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Roles of lithospheric strain softening and heterogeneity in determining the geometry of rifts and continental margins |
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111 | (28) |
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The role of gravitational instabilities, density structure and extension rate in the evolution of continental margins |
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139 | (18) |
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A dynamic model of rifting between Galicia Bank and Flemish Cap during the opening of the North Atlantic Ocean |
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157 | (16) |
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The Iberia-Newfoundland continental extensional system (kinematic modelling) |
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A kinematic modelling approach to lithosphere deformation and basin formation: application to the Black Sea |
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173 | (26) |
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Early kinematic history of the Goban Spur rifted margin derived from a new model of continental breakup and sea-floor spreading initiation |
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199 | (18) |
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Observational characteristics of non-Atlantic extensional systems (offshore) |
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The boundary between continental rifting and sea-floor spreading in the Woodlark Basin, Papua New Guinea |
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217 | (22) |
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Nature of the continent-ocean transition zone along the southern Australian continental margin: a comparison of the Naturaliste Plateau, SW Australia, and the central Great Australian Bight sectors |
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239 | (26) |
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Observational characteristics of non-Atlantic extensional systems (onshore) |
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Constraints on the deformation and rupturing of continental lithosphere of the Red Sea: the transition from rifting to drifting |
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265 | (26) |
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Observations from the Alpine Tethys and Iberia-Newfoundland margins pertinent to the interpretation of continental breakup |
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291 | (34) |
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Overview of tectonic settings related to the rifting and opening of Mesozoic ocean basins in the Eastern Tethys: Oman, Himalayas and Eastern Mediterranean regions |
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325 | (64) |
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Revisiting fundamental concepts of continental extension |
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Continental lithospheric thinning and breakup in response to upwelling divergent mantle flow: application to the Woodlark, Newfoundland and Iberia margins |
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389 | (32) |
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Observations from the Basin and Range Province (western United States) pertinent to the interpretation of regional detachment faults |
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421 | (22) |
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Effects of initial weakness on rift architecture |
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443 | (14) |
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Incompressible viscous formulations for deformation and yielding of the lithosphere |
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457 | (16) |
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| Index |
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473 | |
