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The isotopic and chemical evolution of Mount St....
Journal article

The isotopic and chemical evolution of Mount St. Helens

Abstract

Isotopic and major and trace element analysis of nine samples of eruptive products spanning the history of the Mt. St. Helens volcano suggest three different episodes; (1) 40,000–2500 years ago: eruptions of dacite with εNd = +5, εSr = −10, variable δ18O,206Pb/204Pb ∼ 18.76, Ca/Sr ∼ 60, Rb/Ba ∼ 0.1, La/Yb ∼ 18, (2) 2500-1000 years ago: eruptions of basalt, andesite and dacite with εNd = +4 to +8, εSr = −7 to −22, variable δ18O (thought to …

Authors

Halliday AN; Fallick AE; Dickin AP; Mackenzie AB; Stephens WE; Hildreth W

Journal

Earth and Planetary Science Letters, Vol. 63, No. 2, pp. 241–256

Publisher

Elsevier

Publication Date

May 1983

DOI

10.1016/0012-821x(83)90040-7

ISSN

0012-821X