X Yang, H Gao - Journal of Geophysical Research: Solid Earth, 2020 - Wiley Online Library
The along‐strike variations of the velocity, thickness, and dip of subducting slabs and the volcano distribution have been observed globally. It is, however, unclear what controls the …
Fractures in Earth's critical zone influence groundwater flow and storage and promote chemical weathering. Fractured materials are difficult to characterize on large spatial scales …
For decades, seismic imaging methods have been used to study the critical zone, Earth's thin, life‐supporting skin. The vast majority of critical zone seismic studies use traveltime …
R Trichandi, K Bauer, T Ryberg… - Earth Surface …, 2022 - Wiley Online Library
Imaging the critical zone at depth, where intact bedrock transforms into regolith, is critical in understanding the interaction between geological and biological processes. We acquired a …
The critical zone sustains terrestrial life, but we have few tools to explore it efficiently beyond the first few meters of the subsurface. Using analyses of high‐frequency ambient seismic …
A Roullé, M Baillet, D Bertil… - Comptes …, 2022 - comptes-rendus.academie-sciences …
Since the 2000s, local seismic hazard studies have shown that Mayotte Island presented superficial geological formations prone to lithological site effects. The seismic sequence …
Core Ideas Unsaturated saprolite, saturated saprolite, and fractured rock have unique NMR responses. Surface NMR signals will be dominated by water in saturated saprolite. The …
Y Hu, C Liu, Z Wang, F Zhao - Scientific Reports, 2024 - nature.com
Multistage plate subduction plays a crucial role in magmatism; however, the mechanisms by which deep geodynamic processes govern volcanism in the Alaska subduction zone remain …
W Wang, A Nyblade, G Mount, S Moon… - Journal of …, 2021 - Wiley Online Library
To investigate how bedrock transforms to soil, we mapped the topography of the interface demarcating onset of weathering under an east‐west trending shale watershed in the Valley …