Results 241 to 250 of about 30,017 (275)
Re-Os dating of the Makimine and Shimokawa VMS deposits for new age constraints on ridge subduction beneath Japanese Islands. [PDF]
Sci RepNozaki T, Takaya Y, Nakayama K, Kato Y.
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Full-waveform inversion reveals diverse origins of lower mantle positive wave speed anomalies. [PDF]
Sci RepSchouten TLA +6 more
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Comment on "First finding of continental deep subduction in the Sesia Zone of Western Alps and implications for subduction dynamics". [PDF]
Natl Sci RevCompagnoni R +5 more
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Publisher Correction: Diversities of chromite mineralization induced by chemo-thermal evolution of the mantle during subduction initiation. [PDF]
Nat CommunZhang PF +6 more
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Sluggish thermochemical basal mantle structures support their long-lived stability. [PDF]
Nat CommunShi Z +8 more
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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.
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Devolatilization During Subduction
2014Subducted crust refertilizes the subarc mantle wedge as well as the deep convecting mantle. In the subarc region, mass transfer occurs mainly through fluids, melts, or supercritical liquids. Experiments show that devolatilization reactions may occur at almost any depth in the chemically complex subducting lithosphere.
M. Schmidt, S. Poli
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Annual Review of Earth and Planetary Sciences, 2002
▪ Abstract The subducted lithosphere is composed of a complex pattern of chemical systems that undergo continuous and discontinuous phase transformation, through pressure and temperature variations. Volatile recycling plays a major geodynamic role in triggering mass transfer, melting, and volcanism.
Max W. Schmidt, Stefano Poli
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▪ Abstract The subducted lithosphere is composed of a complex pattern of chemical systems that undergo continuous and discontinuous phase transformation, through pressure and temperature variations. Volatile recycling plays a major geodynamic role in triggering mass transfer, melting, and volcanism.
Max W. Schmidt, Stefano Poli
openaire +3 more sources