Subduction recycling of continental sediments and the origin of geochemically enriched reservoirs in the deep mantle

Earth and Planetary Science Letters

Volumn 271, Issue 1-4, 2008, Pages 14-23

  Rapp, Robert P ^a   Irifune, Tetsuo ^a   Shimizu, Nobu ^b   Nishiyama, Norimasa ^c   Norman, Marc D ^d   Inoue, Toru ^a  

^a EHIME UNIVERSITY   (Japan)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c ARGONNE NATIONAL LABORATORY   (United States)

^d AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

continental sediments; K hollandite; lamproite; mantle transition zone; ocean island basalts (OIB); subduction zones

Indexed keywords

CONTINENTAL (CO); CONTINENTAL CRUSTS; DEEP MANTLE; OCEAN ISLAND BASALT (OIB); TRACE ELEMENT COMPOSITION;

AGRICULTURAL CHEMICALS; BASALT; CHEMICAL ANALYSIS; CHEMICAL ELEMENTS; EARTH SCIENCES; GALLIUM; ISOTOPES; LANDFORMS; LITHOLOGY; MICROFLUIDICS; RECYCLING; RESERVOIRS (WATER); SEDIMENTATION; SEDIMENTOLOGY; TECTONICS;

TRACE ELEMENTS;

ISOTOPIC COMPOSITION; LAMPROITE; MANTLE CHEMISTRY; MARINE SEDIMENT; OCEAN ISLAND BASALT; PHASE EQUILIBRIUM; SUBDUCTION ZONE; TRACE ELEMENT; TRANSITION ZONE;

MYCTEROPERCA FUSCA;

EID: 45049087351     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2008.02.028     Document Type: Article

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