Meteoroid impacts shape planetary surfaces by forming new craters and alter atmospheric
composition. During atmospheric entry and impact on the ground, meteoroids excite …

The Sanriku ocean‐bottom seismometer system uses an optical fiber cable to guarantee
real‐time observations at the seafloor. A dark fiber connected to a Distributed Acoustic …

Seismic waveform modeling is a powerful tool for determining earth structure models and
unraveling earthquake rupture processes, but it is usually computationally expensive. We …

Oceanic lithosphere descends into Earth's mantle at subduction zones and drives material
exchange between Earth's surface and its deep interior. The subduction process creates …

Seismic anisotropy which is common in shale and fractured rocks will cause travel-time and
amplitude discrepancy in different propagation directions. For microseismic monitoring …

The fine-scale seismic features near the inner core boundary (ICB) provide critical insights
into the thermal, chemical, and geodynamical interactions between liquid and solid cores …

Indian continental subduction can explain Cenozoic crustal deformation, magmatic activity
and uplift of the Tibetan Plateau following the India-Asia collision. In the western Himalayan …

The spatial distribution of temporal variations in seismic wavespeed is key to understanding
the sources and physical mechanisms of various geophysical processes. The imaging of …

Surface waves from earthquakes are known to cause strong damage, especially for larger
structures such as skyscrapers and bridges. However, common practice in characterizing …

Seismic waves from earthquakes recorded on the seafloor are composed of complex
multiple arrivals. Here, distributed acoustic sensing (DAS) observations along a cable …