(Q59857997)

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Topography on the 410-km seismic velocity discontinuity near subduction zones from stacking ofsS,sP, andpPprecursors

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Topography on the 410-km seismic velocity discontinuity near subduction zones from stacking ofsS,sP, andpPprecursors (English)

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subduction zone

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Peter M. Shearer

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Peter M. Shearer

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Megan P. Flanagan

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publication date

10 September 1998

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Journal of Geophysical Research

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103

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B9

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21165-21182

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Sharpness of upper-mantle discontinuities determined from high-frequency reflections

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Phase transition Clapeyron slopes and transition zone seismic discontinuity topography

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Mantle discontinuity structure from midpoint stacks of converted P to S waves across the Yellowstone hotspot track

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Preliminary reference Earth model

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Global mapping of topography on transition zone velocity discontinuities by stackingSSprecursors

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A regionalized upper mantle (RUM) seismic model

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Relationship of deep seismicity to the thermal structure of subducted lithosphere

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Double seismic zone for deep earthquakes in the izu-bonin subduction zone

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Seismological evidence for metastable olivine inside a subducting slab

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Hydrous modified spinel, Mg1.75SiH0.5O4: A new water reservoir in the mantle transition region

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The system Mg2SiO4-Fe2SiO4at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel

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Implications of spatial and temporal development of the aftershock sequence for theMw8.3 June 9, 1994 Deep Bolivian Earthquake

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Seismic evidence for silicate melt atop the 410-km mantle discontinuity

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S-Pconversion from the transition zone beneath Tonga and the nature of the 670 km discontinuity

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Seismic imaging of upper-mantle structure with new evidence for a 520-km discontinuity

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Rupture characteristics of the deep bolivian earthquake of 9 june 1994 and the mechanism of deep-focus earthquakes

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Complex morphology of subducted lithosphere in the mantle beneath the Tonga trench

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Tomographic imaging of subducted lithosphere below northwest Pacific island arcs

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based on heuristic

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Upper-mantle seismic discontinuities and the thermal structure of subduction zones

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The 410-km-depth discontinuity: A sharpness estimate from near-critical reflections

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Evidence for transformational faulting from a deep double seismic zone in Tonga

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The Effect of H2O on the 410-Kilometer Seismic Discontinuity

1 reference

https://api.crossref.org/works/10.1029%2F98JB00595

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based on heuristic

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Seismic evidence against a mantle chemical discontinuity near 660 km depth beneath Izu-Bonin

1 reference

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Seismic evidence for very deep roots of continents

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Identifiers

10.1029/98JB00595

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1998JGR...10321165F

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