Crystallisation ages in coeval silicic magma bodies: 238U–230Th disequilibrium evidence from the Rotoiti and Earthquake Flat eruption deposits, Taupo Volcanic Zone, New Zealand-Reference-Cited by-同舟云学术

Crystallisation ages in coeval silicic magma bodies: 238U–230Th disequilibrium evidence from the Rotoiti and Earthquake Flat eruption deposits, Taupo Volcanic Zone, New Zealand

Published:2003-02 Issue:3-4 Volume:206 Page:441-457
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Charlier Bruce L.A,Peate David W,Wilson Colin J.N,Lowenstern Jacob B,Storey Michael,Brown Stuart J.A

Publisher

Elsevier BV

Subject

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

Reference48 articles.

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5. Volcanic and structural evolution of Taupo Volcanic Zone, New Zealand: a review;Wilson;J. Volcanol. Geotherm. Res.,1995

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