Results 221 to 230 of about 114,142 (370)

Several Kilometers of Global Contraction on Mercury: A Sample‐Size Independent Assessment of Fault Strain

open access: yesAGU Advances, Volume 6, Issue 4, August 2025.
Abstract Mercury underwent global contraction due to the sustained cooling of the planet. Positive‐relief landforms, found widespread across Mercury, are thought to be the surface expressions of thrust faults accommodating the contraction. Disagreement exists in the literature on the amount of contraction, with estimates of radius change ranging from ...
Stephan R. Loveless, Christian Klimczak
wiley   +1 more source

Geodynamic evolution of the lithosphere and upper mantle beneath the Alboran region of the western Mediterranean: Constraints from travel time tomography [PDF]

open access: bronze, 2000
Alexander Calvert   +8 more
openalex   +1 more source

Resolution of SWOT Altimetry: Improvements Along Continental Margins

open access: yesEarth and Space Science, Volume 12, Issue 8, August 2025.
Abstract The along‐track sea surface slopes (SSS) computed from the Surface Water and Ocean Topography (SWOT) measurements are extremely important in the retrieval of high‐resolution global marine gravity anomalies. We estimate the spatial resolution of SWOT measurements and assess the inherent improvements offered by wide‐swath altimetry over 12 sites
D. V. P. Krishna, K. M. Sreejith
wiley   +1 more source

Magnetotelluric evidence for highly focused mantle melting along the ultraslow-spreading Gakkel Ridge, Arctic Ocean. [PDF]

open access: yesNatl Sci Rev
Zhang T   +16 more
europepmc   +1 more source

Kinematic Representations of Viscoelastic Postseismic Deformation

open access: yesEarth and Space Science, Volume 12, Issue 8, August 2025.
Abstract Following large earthquakes, viscoelastic stress relaxation may contribute to postseismic deformation observed at Earth's surface. Mechanical representations of viscoelastic deformation require a constitutive relationship for the lower crust/upper mantle material where stresses are diffused and, for non‐linear rheologies, knowledge of absolute
John P. Loveless, Brendan J. Meade
wiley   +1 more source

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