Sources and evolution of arc magmas inferred from coupled O and Hf isotope systematics of plutonic zircons from the Cretaceous Separation Point Suite (New Zealand)-Reference-Cited by-同舟云学术

Sources and evolution of arc magmas inferred from coupled O and Hf isotope systematics of plutonic zircons from the Cretaceous Separation Point Suite (New Zealand)

Published:2008-04 Issue:3-4 Volume:268 Page:312-324
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Bolhar R.,Weaver S.D.,Whitehouse M.J.,Palin J.M.,Woodhead J.D.,Cole J.W.

Publisher

Elsevier BV

Subject

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

Reference70 articles.

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3. Volcanic arc of Kamchatka: a province with high-delta O-18 magma sources and large-scale O-18/O-16 depletion of the upper crust;Bindeman;Geochim. Cosmochim. Acta,2004

4. Oxygen isotope evidence for slab melting in modem and ancient subduction zones;Bindeman;Earth Planet. Sci. Lett.,2005

5. The Largs high-latitude oxygen isotope anomaly (New Zealand) and climatic controls of oxygen isotopes in magma;Blattner;Earth Planet. Sci. Lett.,1991

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