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   https://doi.org/10.1002/2017WR020835  

   Grant, Gordon E.; Dietrich, William E. (April 2017, Water Resources Research)
2. The magmatic web beneath Hawai‘i

   https://doi.org/10.1126/science.ade5755  

   Wilding, John D.; Zhu, Weiqiang; Ross, Zachary E.; Jackson, Jennifer M. (February 2023, Science)

   Interacting magmatic sills at about 40-kilometer depth under the island of Hawai‘i feed into multiple different volcanoes. 

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3. Teleseismic attenuation beneath the British Isles

   https://doi.org/10.1093/gji/ggaf228  

   Zhou, Zhengyang; Bezada, Maximiliano (June 2025, Geophysical Journal International)

   SUMMARY The British Isles' lithospheric structure, shaped by a dynamic geological history, remains incompletely understood, particularly regarding anelastic parameters, such as attenuation. In this study, we present a teleseismic attenuation model for the British Isles, using time-domain analysis of teleseismic P-wave data from 28 deep earthquakes. We constructed a 2-D differential attenuation map (Δt*) that reveals significant regional variations. Our findings show a weak anticorrelation between Δt* and shear wave velocity at upper mantle depths, suggesting that variations in the lithosphere–asthenosphere system influence this pattern. A high-attenuation zone extends from Scotland across the Irish Sea to southwest England, potentially linked to mantle upwelling associated with the Iceland plume. This model provides new insights into the mantle dynamics beneath the British Isles, offering a crucial reference for future geophysical studies in the region. 

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4. Seeing beneath the skin with computational photography

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   Nowara, Ewa; Mcduff, Daniel; Sabharwal, Ashutosh; Veeraraghavan, Ashok (December 2022, Communications of the ACM)

   Optical imaging technologies hold powerful potential in healthcare. 

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5. Mantle flow distribution beneath the California margin

   https://doi.org/10.1038/s41467-020-18260-8  

   Barbot, Sylvain (September 2020, Nature Communications)

   Abstract Although the surface deformation of tectonic plate boundaries is well determined by geological and geodetic measurements, the pattern of flow below the lithosphere remains poorly constrained. We use the crustal velocity field of the Plate Boundary Observatory to illuminate the distribution of horizontal flow beneath the California margin. At lower-crustal and upper-mantle depths, the boundary between the Pacific and North American plates is off-centered from the San Andreas fault, concentrated in a region that encompasses the trace of nearby active faults. A major step is associated with return flow below the Eastern California Shear Zone, leading to the extrusion of the Mojave block and a re-distribution of fault activity since the Pleistocene. Major earthquakes in California have occurred above the regions of current plastic strain accumulation. Deformation is mechanically coupled from the crust to the asthenosphere, with mantle flow overlaid by a kinematically consistent network of faults in the brittle crust. 

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