Hafnium isotope evidence for ‘conservative’ element mobility during subduction zone processes

Author:

Woodhead J.D.,Hergt J.M.,Davidson J.P.,Eggins S.M.

Publisher

Elsevier BV

Subject

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

Reference47 articles.

1. J.A. Pearce, Role of sub-continental lithosphere in magma genesis at active continental margins, in: C.J. Hawkesworth, M.J. Norry (Eds.), Continental Basalts and Mantle Xenoliths, Shiva, Nantwich, 1983, pp. 230–249.

2. Chemical characteristics of a fluid phase from a subducted lithosphere and origin of arc magmas: evidence from high pressure studies and natural rocks;Tatsumi;J. Geophys. Res.,1986

3. Tectonic implications of the compositions of island arc magmas;Pearce;Annu. Rev. Earth Planet. Sci.,1995

4. The mantle source of ocean ridges, island arcs: the Hf-isotope connection;Salters;Earth Planet. Sci. Lett.,1991

5. Hf–Nd–Sr isotopes and incompatible element abundances in island arcs: implications for magma origins and crust–mantle evolution;White;Earth Planet. Sci. Lett.,1984

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