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Rigidity variations with depth along interplate megathrust faults in subduction zones

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Rigidity variations with depth along interplate megathrust faults in subduction zones (English)

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Susan L. Bilek

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Thorne Lay

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Thorne Lay

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English

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publication date

July 1999

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Nature

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volume

400

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issue

6743

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page(s)

443-446

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exact match

https://scigraph.springernature.com/pub.10.1038/22739

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Mechanism of tsunami earthquakes

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Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust

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The 1992 Nicaragua earthquake: a slow tsunami earthquake associated with subducted sediments

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Preliminary reference Earth model

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Variation of interplate fault zone properties with depth in the japan subduction zone

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The depth dependence of earthquake duration and implications for rupture mechanisms

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Time functions of deep earthquakes from broadband and short-period stacks

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The chemical composition of subducting sediment and its consequences for the crust and mantle

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Sediment incorporation in island-arc magmas: Inferences from 10Be

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Tectonic erosion along the Japan and Peru convergent margins

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On the mechanical role of smectite in subduction zones

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Mechanism of the 1992 Nicaragua Tsunami Earthquake

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Crossref

reference URL

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10.1038/22739

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1022975361

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(Q59081698)

Rigidity variations with depth along interplate megathrust faults in subduction zones

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