Plume-lithosphere interactions in rifted margin tectonic settings: Inferences from thermo-mechanical modelling

Autor: François, Thomas, Koptev, Alexander, Cloetingh, Sierd, Burov, Evgueni, Gerya, Taras

Publikováno v: In Tectonophysics 30 October 2018 746:138-154

Plume-induced continental rifting and break-up in ultra-slow extension context: Insights from 3D numerical modeling

Autor: Koptev, Alexander, Burov, Evgueni, Gerya, Taras, Le Pourhiet, Laetitia, Leroy, Sylvie, Calais, Eric, Jolivet, Laurent

Publikováno v: In Tectonophysics 30 October 2018 746:121-137

Afar triple junction triggered by plume-assisted bi-directional continental break-up

Autor: Koptev, Alexander, Gerya, Taras, Calais, Eric, Leroy, Sylvie, Burov, Evgueni

Publikováno v: Scientific Reports
Scientific Reports, 8
Scientific Reports, Nature Publishing Group, 2018, 8 (1), ⟨10.1038/s41598-018-33117-3⟩
Scientific Reports, Vol 8, Iss 1, Pp 1-7 (2018)
Scientific Reports, 2018, 8 (1), ⟨10.1038/s41598-018-33117-3⟩

Divergent ridge-ridge-ridge (R-R-R) triple junctions are one of the most remarkable, yet largely enigmatic, features of plate tectonics. The juncture of the Arabian, Nubian, and Somalian plates is a type-example of the early development stage of a tr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1a428c0a79cdb79eea05d3b9200e05c3
http://europepmc.org/articles/PMC6170478

Asymmetric three-dimensional topography over mantle plumes.

Autor: Burov, Evgueni¹, Gerya, Taras²

Publikováno v: Nature. 9/4/2014, Vol. 513 Issue 7516, p85-89. 5p. 4 Graphs.

Polyphase evolution of continental rifting over active mantle upwelling: Spatial and temporal aspects of transition between wide and narrow rifts

Autor: Koptev, Alexander, Burov, Evgueni, Gerya, Taras, Le Pourhiet, Laetitia, Leroy, Sylvie, Calais, Eric, Jolivet, Laurent

Publikováno v: 19th EGU General Assembly
19th EGU General Assembly, 2017, Vienne, Austria. pp.2670

International audience; The extension of continental lithosphere is usually classified into three modes: narrow rift, wide rift, and core complex. According to previous numerical and analogue experiments, a high-strength lithospheric mantle causes lo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______2417::fd3553aa7d03966bae23d70d4001d0cc
https://hal.science/hal-03552764/file/EGU2017-2670.pdf