Plume-lithosphere interactions in rifted margin tectonic settings: Inferences from thermo-mechanical modelling
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- Type
- article
- Published
- 2017-12-02
- Cited by
- 33
- References
- 90
- Access
- Open access
- OpenAlex
- https://openalex.org/W2773914766
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:133988038
Keywords
Lithosphere, Geology, Mantle plume, Plume, Mantle (geology)
References
- Density structure of the Scandes lithosphere from surface to depth
- Introduction to Numerical Geodynamic Modelling
- Reconstruction of the southwestern African continental margin by backward modeling
- High temperature mechanical behavior of Maryland diabase
- Discretization errors and free surface stabilization in the finite difference and marker‐in‐cell method for applied geodynamics: A numerical study
- Geodynamics : applications of continuum physics to geological problems
- Numerical experiments on localization in frictional materials
- A new parameterization of hydrous mantle melting
- Lithospheric folding and sedimentary basin evolution: a review and analysis of formation mechanisms
- TEMPORAL AND SPATIAL CORRELATIONS BETWEEN CHANGES IN PLATE MOTIONS AND THE EVOLUTION OF RIFTED BASINS IN AFRICA
- Rheology and strength of the lithosphere
- Large uplift of rift flanks: A genetic link with lithospheric rigidity?
- Friction of rocks
- Continental plate collision, P–T–t–z conditions and unstable vs. stable plate dynamics: Insights from thermo-mechanical modelling
- Sedimentary response to mantle plumes: Implications from Paleocene onshore successions, West and East Greenland
- The Moho in extensional tectonic settings: Insights from thermo-mechanical models
- Asymmetric lithospheric extension: The role of frictional plastic strain softening inferred from numerical experiments
- A physical explanation of the relation between flank uplifts and the breakup unconformity at rifted continental margins
- Mechanisms of extensional basin formation and vertical motions at rift flanks: Constraints from tectonic modelling and fission-track thermochronology
- Cenozoic postrift domal uplift of North Atlantic margins: An asthenospheric diapirism model
Cited by
- 1. TITLE OF CONSTITUENT BODY AND NAME OF REPORTERS
- Along‐Axis Variations of Rift Width in a Coupled Lithosphere‐Mantle System, Application to East Africa
- Thermo-mechanical and stratigraphic numerical forward modelling: recent advances and their joint application in the Pannonian Basin
- Quantifying the late-to post-Variscan pervasive heat flow, central Netherlands, Southern Permian Basin
- Radiogenic trigger and driver for continental rifting and initial ocean spreading
- Multiphysics Modeling of a Brittle‐Ductile Lithosphere: 1. Explicit Visco‐Elasto‐Plastic Formulation and Its Numerical Implementation
- The preserved plume of the Caribbean Large Igneous Plateau revealed by 3D data-integrative models
- Plume‐Induced Sinking of Intracontinental Lithospheric Mantle: An Overlooked Mechanism of Subduction Initiation?
- Longevity of small-scale (‘baby’) plumes and their role in lithospheric break-up
- The ‘pargasosphere’ hypothesis: Looking at global plate tectonics from a new perspective
- The Magmatic Architecture of Continental Flood Basalts: 2. A New Conceptual Model
- Plume–MOR decoupling and the timing of India–Eurasia collision
- The role of edge-driven convection in the generation ofvolcanism – Part 2: Interaction with mantle plumes, applied to the Canary Islands
- Quantifying Permanent Uplift Due To Lithosphere‐Hotspot Interaction
- Synchronous exhumation episodes across Arctic Canada, North Greenland and Svalbard in relation to the Eurekan Orogeny
- Plume–ridge interactions: ridgeward versus plate-drag plume flow
- Lithospheric Structure of the Red Sea Based on 3D Density Modeling: A Contrasting Rift Architecture
- Tectono‐Magmatic Evolution of Asymmetric Coronae on Venus: Topographic Classification and 3D Thermo‐Mechanical Modeling
- Two-step exhumation of Caucasian intraplate rifts: A proxy of sequential plate-margin collisional orogenies
- Source‐to‐sink tandem geochronology reveals tectonic influences on the Cambrian Transcontinental Arch of Laurentia
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