Results 251 to 260 of about 74,121 (304)
Bridging the gap between subduction dynamics and the long-term strength of the Sunda megathrust. [PDF]
Nat CommunCapitanio FA +6 more
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Rift linkage and inheritance determine collisional mountain belt evolution. [PDF]
Nat CommunWolf SG, Huismans RS, Muñoz JA, May DA.
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Weak mantle wedge causes mantle exhumation punctuated with discrete oceanic crust in the Tyrrhenian basin. [PDF]
Nat CommunSu H, Leng W, Liao J, Brune S.
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2017
Subduction zones are characterized by multiple behaviors, dynamics, or geometries. Most of them results from the complex interplay between various parameters. In this article, we define the most common parameters used by scientists and then mention the studies where (set of) parameters are tested empirically, or experimentally.
Lallemand, Serge, Heuret, Arnauld
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Subduction zones are characterized by multiple behaviors, dynamics, or geometries. Most of them results from the complex interplay between various parameters. In this article, we define the most common parameters used by scientists and then mention the studies where (set of) parameters are tested empirically, or experimentally.
Lallemand, Serge, Heuret, Arnauld
openaire +1 more source
Creeping subduction zones are weaker than locked subduction zones
Nature Geoscience, 2017Faults that are fully or partially locked pose the greatest seismic hazard because they accumulate stress that can then be released in large earthquakes. In contrast, other faults continuously creep. The creeping versus locked behaviour is probably related to the frictional properties of the fault and the effective normal stress on the fault, but it is
Jeanne L. Hardebeck, John P. Loveless
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Reviews of Geophysics, 2002
Subduction zones are where sediments, oceanic crust, and mantle lithosphere return to and reequilibrate with Earth's mantle. Subduction zones are interior expressions of Earth's 55,000 km of convergent plate margins and are the geodynamic system that builds island arcs.
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Subduction zones are where sediments, oceanic crust, and mantle lithosphere return to and reequilibrate with Earth's mantle. Subduction zones are interior expressions of Earth's 55,000 km of convergent plate margins and are the geodynamic system that builds island arcs.
openaire +1 more source
2009
Subduction Zone Geodynamics.- A Review of the Role of Subduction Dynamics for Regional and Global Plate Motions.- Subduction with Variations in Slab Buoyancy: Models and Application to the Banda and Apennine Systems.- Continental Collision and the STEP-wise Evolution of Convergent Plate Boundaries: From Structure to Dynamics.- Seismic Tomography and ...
Lallemand, Serge, Funiciello, F.
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Subduction Zone Geodynamics.- A Review of the Role of Subduction Dynamics for Regional and Global Plate Motions.- Subduction with Variations in Slab Buoyancy: Models and Application to the Banda and Apennine Systems.- Continental Collision and the STEP-wise Evolution of Convergent Plate Boundaries: From Structure to Dynamics.- Seismic Tomography and ...
Lallemand, Serge, Funiciello, F.
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Physics of the Earth and Planetary Interiors, 2001
Rheological flow laws can be obtained from studies using multi-anvil high-pressure systems with synchrotron-based piezometers and strain metrics. The high flux X-ray source provides minute-scale time resolution with accurate measurement of diffraction patterns and direct sample images. Measurements of length changes with an accuracy of one part in 10 4
Donald J Weidner +5 more
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Rheological flow laws can be obtained from studies using multi-anvil high-pressure systems with synchrotron-based piezometers and strain metrics. The high flux X-ray source provides minute-scale time resolution with accurate measurement of diffraction patterns and direct sample images. Measurements of length changes with an accuracy of one part in 10 4
Donald J Weidner +5 more
openaire +1 more source