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Broad plumes rooted at the base of the Earth's mantle beneath major hotspots
Plumes of hot upwelling rock rooted in the deep mantle have been proposed as a possible
origin of hotspot volcanoes, but this idea is the subject of vigorous debate,. On the basis of …
origin of hotspot volcanoes, but this idea is the subject of vigorous debate,. On the basis of …
Seismic structure of the upper mantle beneath eastern Asia from full waveform seismic tomography
To better understand the subsurface behavior of subducting slabs and their relation to the
tectonic evolution of the overriding plate, we conduct a full waveform inversion on a large …
tectonic evolution of the overriding plate, we conduct a full waveform inversion on a large …
Whole-mantle radially anisotropic shear velocity structure from spectral-element waveform tomography
The radially anisotropic shear velocity structure of the Earth's mantle provides a critical
window on the interior dynamics of the planet, with isotropic variations that are interpreted in …
window on the interior dynamics of the planet, with isotropic variations that are interpreted in …
Solar neutrino measurements in Super-Kamiokande-IV
K Abe, Y Haga, Y Hayato, M Ikeda, K Iyogi, J Kameda… - Physical Review D, 2016 - APS
Upgraded electronics, improved water system dynamics, better calibration and analysis
techniques allowed Super-Kamiokande-IV to clearly observe very low-energy B 8 solar …
techniques allowed Super-Kamiokande-IV to clearly observe very low-energy B 8 solar …
How ocean waves rock the Earth: Two mechanisms explain microseisms with periods 3 to 300 s
Microseismic activity, recorded everywhere on Earth, is largely due to ocean waves. Recent
progress has clearly identified sources of microseisms in the most energetic band, with …
progress has clearly identified sources of microseisms in the most energetic band, with …
Anisotropic shear‐wave velocity structure of the Earth's mantle: A global model
We combine a new, large data set of surface wave phase anomalies, long‐period
waveforms, and body wave travel times to construct a three‐dimensional model of the …
waveforms, and body wave travel times to construct a three‐dimensional model of the …
Inferring upper-mantle temperatures from seismic velocities
Constraints on mantle temperatures are fundamental for a better understanding of the
dynamics of the Earth. We evaluate how well upper-mantle thermal structure can be inferred …
dynamics of the Earth. We evaluate how well upper-mantle thermal structure can be inferred …
Shallow mantle temperatures under Europe from P and S wave tomography
Temperature is one of the key parameters controlling lithospheric and mantle dynamics and
rheology. Using recent experimental data on elastic parameters and anelasticity, we obtain …
rheology. Using recent experimental data on elastic parameters and anelasticity, we obtain …
Multiscale full waveform inversion
We develop and apply a full waveform inversion method that incorporates seismic data on a
wide range of spatio-temporal scales, thereby constraining the details of both crustal and …
wide range of spatio-temporal scales, thereby constraining the details of both crustal and …
A three-dimensional radially anisotropic model of shear velocity in the whole mantle
We present a 3-D radially anisotropic S velocity model of the whole mantle (SAW642AN),
obtained using a large three component surface and body waveform data set and an …
obtained using a large three component surface and body waveform data set and an …