Composition and mass flux of sediment entering the world's subduction zones: Implications for global sediment budgets, great earthquakes, and volcanism-Reference-Cited by-同舟云学术

Composition and mass flux of sediment entering the world's subduction zones: Implications for global sediment budgets, great earthquakes, and volcanism

Published:1996-05 Issue:1-4 Volume:140 Page:1-12
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Rea David K.,Ruff Larry J.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference26 articles.

1. Sediment incorporation in island arc magmas: Inferences from 10Be;Tera;Geochim. Cosmochim. Acta,1986

2. 10Be and 9Be in mineral separates and whole rocks from volcanic arcs: Implications for sediment subduction;Morris;Geochim. Cosmochim. Acta,1989

3. Sediment subduction and magma genesis in the Lesser Antilles: Isotopic and trace element constraints;White;J. Geophys. Res.,1986

4. Multiple sources for basaltic arc rocks from the southern volcanic zone of the Andes (34°–41°S): Trace-element and isotopic evidence for contributions from subducted oceanic crust, mantle, and continental crust;Hickey;J. Geophys. Res.,1986

5. Tracing trace elements from sediment input to volcanic output at subduction zones;Plank;Nature,1993

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