Results 21 to 30 of about 9,129 (164)

Patched removal of the mantle lithosphere under orogens: A systematic numerical study

open access: yesFrontiers in Earth Science, 2023
Delamination or convective thinning could cause large-scale and complete removal of the mantle lithosphere under orogens. However, geological and geophysical observations suggest that patched removal of the mantle lithosphere has occurred in some orogens,
Tian Lei   +6 more
doaj   +1 more source

A subduction influence on ocean ridge basalts outside the Pacific subduction shield

open access: yesNature Communications, 2021
We discover a pervasive subduction influence in the Arctic, Atlantic and Indian mantle, which is nearly absent in the Pacific mantle. Such a hemispheric-scale upper mantle heterogeneity reflects the control of a “subduction shield” that has surrounded ...
A. Y. Yang   +5 more
doaj   +1 more source

Geochemical Constraints on the Structure of the Earth's Deep Mantle and the Origin of the LLSVPs

open access: yesGeochemistry, Geophysics, Geosystems, 2021
Geophysical analysis of the Earth's lower mantle has revealed the presence of two superstructures characterized by low shear wave velocities on the core‐mantle boundary.
Matthew Gleeson   +4 more
doaj   +1 more source

Low‐Degree Melt Metasomatic Origin of Global Upper Mantle Fe Isotope Fractionation

open access: yesGeophysical Research Letters, 2023
The upper mantle is heterogeneous in Fe isotope compositions, but the origin of the heterogeneity needs understanding. Recent studies on oceanic basalts demonstrate that the upper mantle Fe isotope heterogeneity results from low‐degree melt metasomatism.
Pengyuan Guo   +7 more
doaj   +1 more source

Viscoelastic Mantle Density Heterogeneity and Core-Mantle Topograph [PDF]

open access: yesGeophysical Journal International, 1996
SUMMARY Starting with the model of mantle density heterogeneity derived by Ricard et al. (1993), which uses plate-motion reconstructions under the assumption that subducted slabs sink vertically into the mantle, we model the temporal evolution of these internal loads.
Marianne Greff-Lefftz, Hilaire Legros
openaire   +1 more source

Tomography of core-mantle boundary and lowermost mantle coupled by geodynamics: joint models of shear and compressional velocity

open access: yesAnnals of Geophysics, 2015
We conduct joint tomographic inversions of P and S travel time observations to obtain models of delta v_P  and delta v_S in the entire mantle. We adopt a recently published method which takes into account the geodynamic coupling between mantle ...
Gaia Soldati   +3 more
doaj   +1 more source

Competing effects of spreading rate, crystal fractionation and source variability on Fe isotope systematics in mid-ocean ridge lavas

open access: yesScientific Reports, 2021
Two-thirds of the Earth is covered by mid-ocean ridge basalts, which form along a network of divergent plate margins. Basalts along these margins display a chemical diversity, which is consequent to a complex interplay of partial mantle melting in the ...
Marianne Richter   +4 more
doaj   +1 more source

Global observations of reflectors in the mid-mantle with implications for mantle structure and dynamics

open access: yesNature Communications, 2018
The Earth’s mantle undergoes changes as temperature and pressure increase with depth. Here, the authors present a global interrogation of reflectors in the Earth’s mid-mantle revealing a significant variation in their properties, with widespread ...
Lauren Waszek   +2 more
doaj   +1 more source

pyMelt: An extensible Python engine for mantle melting calculations

open access: yesVolcanica, 2022
Modelling the melting of Earth’s mantle is crucial for understanding the distribution of volcanic activity on Earth and for testing models of mantle convection and mantle lithological heterogeneity.
Simon Matthews   +2 more
doaj   +1 more source

Dense hydrous silica carrying water to the deep Earth and promotion of oxygen fugacity heterogeneity

open access: yesMatter and Radiation at Extremes, 2022
Water has remarkable effects on the properties of mantle rocks, but, owing to the high temperatures in the mantle, uncertainties remain about how and how much water is transported into the deep Earth.
Yanhao Lin, Ho-Kwang Mao
doaj   +1 more source

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