Results 161 to 170 of about 17,328 (228)
Abstract The interaction between the Tethyan and Paleo‐Pacific subduction systems in Southeast Asia since the Paleozoic is still poorly understood. Hainan Island and Borneo, located near the junction of the Tethyan and Paleo‐Pacific domains, provide the critical regions for understanding the dynamic processes and interaction between the two tectonic ...
Yang Zhou +14 more
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Anatomy of a post-subduction collision. [PDF]
Şengül Uluocak E +3 more
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Abstract Postseismic afterslip has been inferred to occur on fault barriers surrounding coseismic asperities, which can be explained by velocity‐strengthening friction in barriers and velocity‐weakening friction in asperities. However, afterslip also exhibits spatial overlap with coseismic slip for some events.
Yuan Gao +10 more
wiley +1 more source
Sublithospheric diamond constraints on the state of deeply subducted slabs. [PDF]
Zhang Q +11 more
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Mantle deformation records fossil convergent upwelling at Perm Anomaly. [PDF]
Wolf J, Li M, Romanowicz B.
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Deep mantle anomalies block early Earth melting, challenging a primordial origin. [PDF]
Roy A, Mittelstaedt E, Cooper CM.
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Mantle melting and lithospheric structure beneath eastern Australia's Cenozoic volcanoes from 3D magnetotellurics. [PDF]
Margiono R, Heinson G.
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Zinc isotope evidence for extensive carbonate recycling in the Arctic asthenosphere. [PDF]
Zhang WQ +11 more
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Himalayan sub-Moho earthquakes suggest crustal faults trigger eclogitized-drip tectonics. [PDF]
Song X, Klemperer SL.
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Rheology of the Upper Mantle: A Synthesis
Science, 1993Rheological properties of the upper mantle of the Earth play an important role in the dynamics of the lithosphere and asthenosphere. However, such fundamental issues as the dominant mechanisms of flow have not been well resolved. A synthesis of laboratory studies and geophysical and geological observations shows that transitions between diffusion and ...
Shun-Ichiro Karato, Patrick Wu
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