Water‐rock interactions within the seafloor are responsible for significant energy and solute
fluxes between basaltic oceanic crust and the overlying ocean. Permeability is the primary …

Pn data collected within southern Europe and the Mediterranean are used to
tomographically image variations in both seismic velocity and seismic anisotropy. Seismic …

The crustal structure across the Tonga‐Lau arc‐back arc system from the Lau Ridge to the
Pacific Plate (178°–170° W, 18° 19° S) is modeled, using data from an 840‐km‐long air gun …

Seafloor compliance measurements across the East Pacific Rise at 9° 48′ N reveal low
shear velocities throughout the crust and at the crust‐mantle boundary, with the lowest shear …

We have determined the three‐dimensional P wave velocity structure and azimuthal
anisotropy within the shallow crust of the inner valley at the Mid‐Atlantic Ridge (MAR) near …

C.-F. Li, J. Lin, DK Kulhanek, T. Williams, R. Bao, A. Briais, EA Brown, Y. Chen, PD Clift, FS
Colwell, KA Dadd, W.-W. Ding, I. Hernández-Almeida, X.-L. Huang, S. Hyun, T. Jiang, AAP …

Axial volcano, which is located near the intersection of the Juan de Fuca ridge and the Cobb–
Eickelberg seamount chain beneath the northeast Pacific Ocean, is a locus of volcanic …

Marine hydrogeology is a broad-ranging scientific discipline involving the exploration of fluid–
rock interactions below the seafloor. Studies have been conducted at seafloor spreading …

Subseafloor hydrologic observatories (CORKs) were installed in four boreholes in young
seafloor on the eastern flank of the Juan de Fuca ridge to evaluate the hydrogeology of the …

The seismic anisotropy of the shallow oceanic crust across the East Pacific Rise (9° 30′ N)
is studied with P-wave refraction data collected during a controlled-source, three …