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Surface waves and crustal structure on Mars
We detected surface waves from two meteorite impacts on Mars. By measuring group
velocity dispersion along the impact-lander path, we obtained a direct constraint on crustal …
velocity dispersion along the impact-lander path, we obtained a direct constraint on crustal …
Crustal anisotropy in the Martian lowlands from surface waves
The largest seismic event ever recorded on Mars, with a moment magnitude of 4.7±0.2, is
the first event to produce both Love and Rayleigh wave signals. We measured their group …
the first event to produce both Love and Rayleigh wave signals. We measured their group …
Different Martian crustal seismic velocities across the dichotomy boundary from multi‐orbiting surface waves
We have observed both minor‐arc (R1) and major‐arc (R2) Rayleigh waves for the largest
marsquake (magnitude of 4.7±0.2) ever recorded. Along the R1 path (in the lowlands) …
marsquake (magnitude of 4.7±0.2) ever recorded. Along the R1 path (in the lowlands) …
EARA2024: a new radially anisotropic seismic velocity model for the crust and upper mantle beneath East Asia and Northwestern pacific subduction zones
We present a new 3-D radially anisotropic seismic velocity model EARA2024 of the crust
and mantle beneath East Asia and the northwestern Pacific using adjoint full-waveform …
and mantle beneath East Asia and the northwestern Pacific using adjoint full-waveform …
Deep geophysical anomalies beneath the Changbaishan volcano
Subsurface imaging is key to understanding the origin of intraplate volcanoes. The
Changbaishan volcano, located about 2,000 km away from the western Pacific subduction …
Changbaishan volcano, located about 2,000 km away from the western Pacific subduction …
Constraining the 410-km discontinuity and slab structure in the Kuril subduction zone with triplication waveforms
The detailed structure near the 410-km discontinuity provides key constraints of the dynamic
interactions between the upper mantle and the lower mantle through the mantle transition …
interactions between the upper mantle and the lower mantle through the mantle transition …
Ultra-low-velocity anomaly inside the Pacific Slab near the 410-km discontinuity
The upper boundary of the mantle transition zone, known as the “410-km discontinuity”, is
attributed to the phase transformation of the mineral olivine (α) to wadsleyite (β olivine). Here …
attributed to the phase transformation of the mineral olivine (α) to wadsleyite (β olivine). Here …
Deep geophysical anomalies beneath the Changbaishan Volcano
Subsurface imaging is key to understanding the origin of intraplate volcanos. The
Changbaishan volcano, located about 2000 km away from the western Pacific subduction …
Changbaishan volcano, located about 2000 km away from the western Pacific subduction …