(Q64013029)

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Hydrous minerals in the mantle wedge and the maximum depth of subduction thrust earthquakes

scholarly article by Simon M. Peacock & Roy D. Hyndman published 15 August 1999 in Geophysical Research Letters

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Hydrous minerals in the mantle wedge and the maximum depth of subduction thrust earthquakes (English)

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Roy D. Hyndman

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author name string

Simon M. Peacock

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1

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publication date

15 August 1999

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number of pages

4

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Geophysical Research Letters

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volume

26

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issue

16

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page(s)

2517-2520

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cites work

Fluid flow and metasomatism in a subduction zone hydrothermal system: Catalina Schist terrane, California

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7 January 2021

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Structure of an island-arc: Wide-angle seismic studies in the eastern Aleutian Islands, Alaska

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An internally consistent thermodynamic data set for phases of petrological interest

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7 January 2021

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The seismogenic zone of subduction thrust faults

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The updip and downdip limits to great subduction earthquakes: Thermal and structural models of Cascadia, south Alaska, SW Japan, and Chile

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Fluid processes in subduction zones

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Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation

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7 January 2021

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Serpentine stability to mantle depths and subduction-related magmatism

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7 January 2021

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

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(Q64013029)

Hydrous minerals in the mantle wedge and the maximum depth of subduction thrust earthquakes

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