Articles | Volume 12, issue 3
https://doi.org/10.5194/se-12-613-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-613-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Mar 2021
Research article |
| 10 Mar 2021
| 10 Mar 2021
The role of edge-driven convection in the generation of volcanism – Part 1: A 2D systematic study
Antonio Manjón-Cabeza Córdoba
CORRESPONDING AUTHOR
Department of Earth Sciences, Institute of Geophysics, ETH, 8092 Zürich, Switzerland
Maxim D. Ballmer
Department of Earth Sciences, Institute of Geophysics, ETH, 8092 Zürich, Switzerland
Department of Earth Sciences, University College, London, WC1E 6BS, UK
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17 citations as recorded by crossref.
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- Geodynamic Controls on Basaltic Volcanism in the Arabian Peninsula: Evolution of Harrat Uwayrid, Saudi Arabia S. Bowden et al. 10.1029/2022GC010780
- Multi-scale anisotropy in NE China: Evidence for localized mantle upwelling C. Han et al. 10.1016/j.epsl.2023.118495
- Edge-driven asthenospheric convection beneath the North China Craton: A numerical study Y. Sun & M. Liu 10.1016/j.tecto.2023.229726
- Geodynamic studies of southwestern Canada: subduction zone processes and backarc mantle dynamics C. Currie & T. Yu 10.1139/cjes-2022-0140
- The role of edge-driven convection in the generation ofvolcanism – Part 2: Interaction with mantle plumes, applied to the Canary Islands A. Manjón-Cabeza Córdoba & M. Ballmer 10.5194/se-13-1585-2022
- Linking Intraplate Volcanism to Lithospheric Structure and Asthenospheric Flow T. Duvernay et al. 10.1029/2021GC009953
- The Twihinate carbonatite (Moroccan Sahara): Evidence for compositional mantle heterogeneity and northwestern African plate geodynamics W. Boukirou et al. 10.1016/j.chemgeo.2023.121648
- Geophysical evidence for an active mantle plume underneath Elysium Planitia on Mars A. Broquet & J. Andrews-Hanna 10.1038/s41550-022-01836-3
- Electrical resistivity structure across the Late Cenozoic Abaga-Dalinor volcanic field, eastern China, from 3-D magnetotelluric imaging and its tectonic implications Z. Dong et al. 10.1016/j.jseaes.2023.105574
- Sub‐Lithospheric Small‐Scale Convection Tomographically Imaged Beneath the Pacific Plate Z. Eilon et al. 10.1029/2022GL100351
- Longevity of small-scale (‘baby’) plumes and their role in lithospheric break-up A. Koptev et al. 10.1093/gji/ggab223
- The Origin of the Low‐Velocity Anomalies Beneath the Rootless Atlas Mountains: Insights Gained From Modeling of Anisotropy Developed by the Travel of Canary Plume H. Lee et al. 10.1029/2022JB024622
- The Mechanical Nature of the Lithosphere Beneath the Eastern Central Atlantic Hotspots A. Jiménez‐Díaz et al. 10.1029/2022GC010608
- Isotopic constraints on Davis bank, Vitória-Trindade Ridge: A Revised Petrogenetic Model G. de Oliveira Amaral Quaresma et al. 10.1016/j.jsames.2022.104099
- The Role of the Seismically Slow Central‐East Atlantic Anomaly in the Genesis of the Canary and Madeira Volcanic Provinces C. Civiero et al. 10.1029/2021GL092874
- Mantle structure beneath the Macaronesian volcanic islands (Cape Verde, Canaries, Madeira and Azores): A review and future directions C. Civiero et al. 10.3389/feart.2023.1126274
15 citations as recorded by crossref.
- On the origin of the Canary Islands: Insights from mantle convection modelling A. Negredo et al. 10.1016/j.epsl.2022.117506
- Geodynamic Controls on Basaltic Volcanism in the Arabian Peninsula: Evolution of Harrat Uwayrid, Saudi Arabia S. Bowden et al. 10.1029/2022GC010780
- Multi-scale anisotropy in NE China: Evidence for localized mantle upwelling C. Han et al. 10.1016/j.epsl.2023.118495
- Edge-driven asthenospheric convection beneath the North China Craton: A numerical study Y. Sun & M. Liu 10.1016/j.tecto.2023.229726
- Geodynamic studies of southwestern Canada: subduction zone processes and backarc mantle dynamics C. Currie & T. Yu 10.1139/cjes-2022-0140
- The role of edge-driven convection in the generation ofvolcanism – Part 2: Interaction with mantle plumes, applied to the Canary Islands A. Manjón-Cabeza Córdoba & M. Ballmer 10.5194/se-13-1585-2022
- Linking Intraplate Volcanism to Lithospheric Structure and Asthenospheric Flow T. Duvernay et al. 10.1029/2021GC009953
- The Twihinate carbonatite (Moroccan Sahara): Evidence for compositional mantle heterogeneity and northwestern African plate geodynamics W. Boukirou et al. 10.1016/j.chemgeo.2023.121648
- Geophysical evidence for an active mantle plume underneath Elysium Planitia on Mars A. Broquet & J. Andrews-Hanna 10.1038/s41550-022-01836-3
- Electrical resistivity structure across the Late Cenozoic Abaga-Dalinor volcanic field, eastern China, from 3-D magnetotelluric imaging and its tectonic implications Z. Dong et al. 10.1016/j.jseaes.2023.105574
- Sub‐Lithospheric Small‐Scale Convection Tomographically Imaged Beneath the Pacific Plate Z. Eilon et al. 10.1029/2022GL100351
- Longevity of small-scale (‘baby’) plumes and their role in lithospheric break-up A. Koptev et al. 10.1093/gji/ggab223
- The Origin of the Low‐Velocity Anomalies Beneath the Rootless Atlas Mountains: Insights Gained From Modeling of Anisotropy Developed by the Travel of Canary Plume H. Lee et al. 10.1029/2022JB024622
- The Mechanical Nature of the Lithosphere Beneath the Eastern Central Atlantic Hotspots A. Jiménez‐Díaz et al. 10.1029/2022GC010608
- Isotopic constraints on Davis bank, Vitória-Trindade Ridge: A Revised Petrogenetic Model G. de Oliveira Amaral Quaresma et al. 10.1016/j.jsames.2022.104099
2 citations as recorded by crossref.
- The Role of the Seismically Slow Central‐East Atlantic Anomaly in the Genesis of the Canary and Madeira Volcanic Provinces C. Civiero et al. 10.1029/2021GL092874
- Mantle structure beneath the Macaronesian volcanic islands (Cape Verde, Canaries, Madeira and Azores): A review and future directions C. Civiero et al. 10.3389/feart.2023.1126274
Latest update: 26 Apr 2024
Short summary
The study of intraplate volcanism can inform us about underlying mantle dynamic processes and thermal and/or compositional anomalies. Here, we investigated numerical models of mantle flow and melting of edge-driven convection (EDC), a potential origin for intraplate volcanism. Our most important conclusion is that EDC can only produce moderate amounts of mantle melting. By itself, EDC is insufficient to support the formation of voluminous island-building volcanism over several millions of years.
The study of intraplate volcanism can inform us about underlying mantle dynamic processes and...
