Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
Descrição
Possible chemical leftovers from early Earth
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://media.springernature.com/w136h75/springer-static/image/art%3A10.1038%2Fs41467-023-37067-x/MediaObjects/41467_2023_37067_Fig1_HTML.png)
Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://www.science.org/cms/10.1126/sciadv.add4838/asset/983a7710-1799-4bd4-8a09-42a622dc3d4b/assets/images/large/sciadv.add4838-f6.jpg)
Globally distributed subducted materials along the Earth's core-mantle boundary: Implications for ultralow velocity zones
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://media.springernature.com/m685/springer-static/image/art%3A10.1007%2Fs11214-023-00995-7/MediaObjects/11214_2023_995_Fig10_HTML.png)
Magma Ocean, Water, and the Early Atmosphere of Venus
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://www.pnas.org/cms/10.1073/pnas.1519540113/asset/13df94f8-cd98-4c32-a6bc-c2e60c7228d5/assets/graphic/pnas.1519540113fig02.jpeg)
Origins of ultralow velocity zones through slab-derived metallic melt
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://www.geo-down-under.org.au/content/images/2023/01/2022_retro.png)
2022, IN A NUTSHELL
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://www.pnas.org/cms/asset/77ce0c44-8f08-46fd-9947-30db1024611d/keyimage.jpg)
Compositional and thermal state of the lower mantle from joint 3D inversion with seismic tomography and mineral elasticity
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://media.springernature.com/m685/springer-static/image/art%3A10.1186%2Fs40645-020-00327-1/MediaObjects/40645_2020_327_Figa_HTML.png)
Subducted oceanic crust as the origin of seismically slow lower-mantle structures, Progress in Earth and Planetary Science
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://agupubs.onlinelibrary.wiley.com/cms/asset/e0fd4c84-278e-496b-b13b-5dfe18e1e83f/ggge.v24.6.cover.jpg?trick=1698975850207)
Lowermost Mantle Structure Beneath the Central Pacific Ocean: Ultralow Velocity Zones and Seismic Anisotropy - Wolf - 2023 - Geochemistry, Geophysics, Geosystems - Wiley Online Library
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://www.researchgate.net/publication/357443267/figure/fig2/AS:1106943557025792@1640927318839/Stacked-ScP-waveforms-a-Stack-of-deconvolved-ScP-waveforms-black-lines-with-stacked_Q320.jpg)
Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
![Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean](https://d3i71xaburhd42.cloudfront.net/80fcf9a03d97228c02a3f38291bb62179fcdea0d/2-Figure1-1.png)
PDF] Tracking deep mantle reservoirs with ultra-low velocity zones
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