Inverse Correlation Between Radiogenic Isotopes and Trace Element Enrichment in Subduction Rocks from New Zealand: The Case for a Four Component Model

C. Münker
Institut für Geologie und Dynamik der Lithosphäre and Geochemisches Institut, Goldsehmidtstr. 3, 37077 Göttingen, Germany

Mineralogical Magazine; 1998 v. 62A; no. 2; p. 1040-1041; DOI: 10.1180/minmag.1998.62A.2.211
© 1998, The Mineralogical Society
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