Results 221 to 230 of about 114,142 (370)
A Countercurrent Accompanying the Descending Pacific Lithosphere (3)
Takuzo Hirono
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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
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Wholesale flat subduction of the Indian slab and northward mantle convective flow: Plateau growth and driving force of the India-Asia collision. [PDF]
Ma J+4 more
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Geodynamic evolution of the lithosphere and upper mantle beneath the Alboran region of the western Mediterranean: Constraints from travel time tomography [PDF]
Alexander Calvert+8 more
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Resolution of SWOT Altimetry: Improvements Along Continental Margins
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
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Magnetotelluric evidence for highly focused mantle melting along the ultraslow-spreading Gakkel Ridge, Arctic Ocean. [PDF]
Zhang T+16 more
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Observations of flexure and the rheology of oceanic lithosphere [PDF]
A. B. Watts, Shijie Zhong
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Kinematic Representations of Viscoelastic Postseismic Deformation
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
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