Hf-Nd isotope variation in Mariana Trough basalts: The importance of "ambient mantle" in the interpretation of subduction zone magmas

Geology

Volumn 40, Issue 6, 2012, Pages 539-542

  Woodhead, Jon ^a   Stern, Robert J ^b   Pearce, Julian ^c   Hergt, Janet ^a   Vervoort, Jeff ^d  

^a UNIVERSITY OF MELBOURNE   (Australia)

^b UNIVERSITY OF TEXAS AT DALLAS   (United States)

^c CARDIFF UNIVERSITY   (United Kingdom)

^d WASHINGTON STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ALTERNATIVE APPROACH; BACK-ARC BASIN; HF ISOTOPE; HIGHLY-CORRELATED; ISOTOPE VARIATION; ISOTOPICALLY ENRICHED; LOCAL SCALE; MANTLE WEDGE; MASS BALANCE; MID-OCEANIC-RIDGE BASALTS; MOBILE ELEMENTS; ND ISOTOPES; SUBDUCTION ZONE MAGMAS; SUBDUCTION ZONES;

GEOCHEMISTRY; HAFNIUM; NEODYMIUM; VOLCANOES;

ISOTOPES;

BACKARC BASIN; GEOCHEMISTRY; HAFNIUM; ISOTOPIC COMPOSITION; LAVA; MID-OCEAN RIDGE BASALT; NEODYMIUM ISOTOPE; SUBDUCTION ZONE;

MARIANA TROUGH; PACIFIC OCEAN;

EID: 84864319119     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/G32963.1     Document Type: Article

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