Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Paul James Tackley"'
Publikováno v:
eISSN
The long-term evolution of the mantle is simulated using 2D spherical annulus geometry to examine the effect of heterogeneous thermal conductivity on the stability of reservoirs of primordial material. Often in numerical models, purely depth-dependen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::da1086840d30312a4ee07928cddeaa9d
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-418/
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-418/
Publikováno v:
Solid Earth, 14 (2)
The long-term evolution of the mantle is simulated using 2D spherical annulus geometry to examine the effect of heterogeneous thermal conductivity on the stability of reservoirs of primordial material. Often in numerical models, purely depth-dependen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d10260c60a0c3ef52d273e03fbceacb
https://hdl.handle.net/20.500.11850/601346
https://hdl.handle.net/20.500.11850/601346
Publikováno v:
Solid Earth, 12 (9)
The nature of compositional heterogeneity in Earth's lower mantle remains a long-standing puzzle that can inform about the long-term thermochemical evolution and dynamics of our planet. Here, we use global-scale 2D models of thermochemical mantle con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4ebcaabbafc5277be94b4a4666abd495
https://doi.org/10.5194/se-2020-205
https://doi.org/10.5194/se-2020-205
Autor:
Daniela Paz Bolrão, Maxim Dionys Ballmer, Adrien Morison, Antoine Billy Rozel, Patrick Sanan, Stéphane Labrosse, Paul James Tackley
After accretion and formation, terrestrial planets go through at least one magma ocean episode. As the magma ocean crystallises, it creates the first layer of solid rocky mantle. Two different scenarios of magma ocean crystallisation involve that the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::739cb5638bd11f976d4efdd246fc3a6a
https://doi.org/10.5194/se-2020-49
https://doi.org/10.5194/se-2020-49