Lateral variation of upper mantle structure beneath New Caledonia determined from P-wave receiver function: evidence for a fossil subduction zone [PDF]
Marc Régnier
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: The recent proposition for a long-lived (635-580 Ma) magmatic arc in the central portion of the Borborema Province is critically evaluated. Evidence favoring subduction include: low-T, high-P metamorphism; local occurrence of retroeclogites; and the ...
Sérgio Pacheco Neves
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Keybarkuh area is located 70 km southwest of Khaf, Khorasan Razavi province. The study area is situated in northeastern Lut block. The rock units in the area are Paleozoic metamorphic rocks and Cretaceous to Tertiary subvolcanic intrusions intruded as ...
Ehsan Salati+5 more
doaj
Introduction The occurrence of blueschist metamorphic facies is believed to mark the existence of former subduction zones. This facies is represented in the main constituents of subduction-accretion complexes, where it occurs in separate tectonic ...
Fereshteh Bayat, Ghodrat Torabi
doaj
Cycling of sulfur in subduction zones: The geochemistry of sulfur in the Mariana Island Arc and back-arc trough [PDF]
Jeffrey C. Alt+2 more
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A systematic search for tectonic tremor and low-frequency earthquakes in the Atacama segment of the Chilean subduction zone (24$^\circ$S-31$^\circ$S) turns up empty [PDF]
Subduction megathrusts release stress not only seismically through earthquakes, but also through creep and transient slow deformation, called slow slip events (SSEs). Understanding the interplay between fast and slow slip is essential for illuminating the deformation processes on the subduction interface. The Chilean subduction margin, while one of the
arxiv
A PRELIMINARY THERMAL MODEL OF THE MEXICAN SEISMOVOLCANIC BELT AS A RESULT OF SUBDUCTION
E. A. Lubimova
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Editorial: Seeing convergent margin processes through metamorphism
Yi Chen+6 more
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Seismological evidence for a discontinuity In subduction zones
Cinna Lomnitz
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Earthquake source processes and subduction regime in the Santa Cruz Islands region [PDF]
Fumiko Tajima+4 more
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