Results 51 to 60 of about 9,129 (164)
Unraveling the Connection Between Subsurface Stress and Geomorphic Features
The tectonic stress field induces surface deformation. At long wavelengths, both lithospheric heterogeneity (changes in the thickness and density of crust and lithospheric mantle) and basal tractions from mantle convection contribute to the stress field.
B. Kuhasubpasin +2 more
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Earth’s mantle isotopic composition is highly heterogeneous, with enriched and depleted regions1–3 shaped by a complex history of depletion and re-enrichment over 4.5 billion years.
Piero A. B. de Sampaio +2 more
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Mantle heterogeneity caused by trapped water in the Southwest Basin of the South China Sea. [PDF]
Tian J +8 more
europepmc +1 more source
The volcanic complex of Mts. Cimini (~0.90-1.30Ma) represents the geographical and chronological transition between the Tuscan Magmatic Province (TMP) and the Roman Magmatic Province (RMP), in central Italy.
M. AULINAS +5 more
doaj
How P‐Wave Scattering Throughout the Entire Mantle Mimics the High‐Frequency Pdiff and Its Coda
We document the arrival of seismic energy in the core shadow zone up to large distances beyond 150° more than 100 s prior to the core phases. Numerical simulations of the energy transport in an established heterogeneity model show that scattering ...
Tuo Zhang +3 more
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We collected approximately 500 ScS–S differential travel times passing beneath the Philippines with various azimuths to discuss whether there were azimuthal variations in the ScS–S time residuals.
Satoru Tanaka
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Is the Deep Martian Mantle Heterogeneous? A Reappraisal of Seismological Evidences
It has been proposed that the deep Martian mantle contains distributed heterogeneities preserved since the accretion of the planet. This result relies on a multiple‐scattering interpretation of frequency‐dependent arrival times of P‐waves detected in the
L. Margerin
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Evidences for mantle heterogeneities in the western Mediterranean
Goldschmidt 2015, 16.08 - 21.08.2015 , Prague, Czech ...
Melchiorre, Massimiliano +5 more
openaire +2 more sources
Impact of Mantle Velocity Uncertainty on Receiver‐Function Imaging of the Transition Zone
Seismological estimates of the 400‐km and 670‐km mantle discontinuities (d400 and d670) are crucial for understanding the thermochemical structure and dynamics of the mantle transition zone (MTZ).
Carlos A. M. Chaves +2 more
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