The effect of sediment recycling in subduction zones on the Hf isotope character of new arc crust, Banda arc, Indonesia

Earth and Planetary Science Letters

Volumn 303, Issue 3-4, 2011, Pages 240-250

  Nebel, O ^a,b   Vroon, P Z ^a   van Westrenen, W ^a   Iizuka, T ^b   Davies, G R ^a  

^a VU UNIVERSITY AMSTERDAM   (Netherlands)

^b AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Banda arc; Hadaean subduction; Hf O isotopes; Zircon

Indexed keywords

ARC MAGMAS; BANDA ARC; CO-VARIATIONS; CONCENTRATION DATA; CONTINENTAL MATERIALS; CONVERGENT MARGIN; CONVERGENT PLATE BOUNDARIES; EARTH'S CRUST; HADAEAN SUBDUCTION; HF ISOTOPE; HF-O ISOTOPES; HIGH-PRECISION; INDONESIA; ISOTOPE GEOCHEMISTRY; ND ISOTOPES; PARTIAL MELTING; PB ISOTOPES; SEDIMENT RECYCLING; SUBDUCTION ZONES; SURFACE TEMPERATURES;

ANOXIC SEDIMENTS; EXPLORATORY GEOCHEMISTRY; ISOTOPES; LEAD; MELTING; NEODYMIUM; RECYCLING; ROCKS; SEDIMENTOLOGY; SILICATE MINERALS; STRONTIUM; STRUCTURAL GEOLOGY; TRACE ELEMENTS; VOLCANIC ROCKS; ZIRCON; ZIRCONIUM;

HAFNIUM;

CONCENTRATION (COMPOSITION); CRUSTAL RECYCLING; HADEAN; HAFNIUM; IGNEOUS GEOCHEMISTRY; ISOTOPIC COMPOSITION; MANTLE SOURCE; OCEANIC CRUST; OXYGEN ISOTOPE; PARTIAL MELTING; SUBDUCTION ZONE; ZIRCON;

BANDA ARC; INDONESIAN SEAS; PACIFIC OCEAN;

EID: 79952103359     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2010.12.053     Document Type: Article

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