HR: 11:20h
AN: V12A-05    [Abstracts]
TI: A New Hygrometer based on the Europium Anomaly in Clinopyroxene Phenocrysts in Arc Volcanic Rocks
AU: * Plank, T
EM: tplank@bu.edu
AF: Boston Univ., Dept Earth Sci., 685 Commonwealth Ave, Boston, MA 02215
AU: Benjamin, E
EM: ezra.benjamin@erm.com
AF: Boston Univ., Dept Earth Sci., 685 Commonwealth Ave, Boston, MA 02215
AU: Wade, J
EM: jwade@bu.edu
AF: Boston Univ., Dept Earth Sci., 685 Commonwealth Ave, Boston, MA 02215
AU: Grove, T
EM: tlgrove@MIT.EDU
AF: MIT, Dept of Earth, Atm, Planet Sci., 54-1220, Cambridge, MA 02139
AB: Water is arguably the most important chemical component in arc magmas, affecting everything from liquidus temperatures to crystal fractionation trends to melt rheology. Water concentrations in arc magmas provide a first-order constraint on water contents in the mantle wedge, and the mechanisms of wet mantle melting. However, measuring the water content of primary arc magmas has been difficult, or in some cases impossible, due to the near complete degassing of volcanic rocks, and the scarcity of olivine-hosted melt inclusions in many arc volcanoes. We have thus developed a new hygrometer using the composition of clinopyroxene phenocrysts, which are common in arc basalts and andesites. The hygrometer is based on the well-known suppression of plagioclase by water dissolved in the melt, and the effect on the rare earth element (REE) pattern of coexisting phases, such as clinopyroxene. Dry melts saturate in plagioclase early, and the preferential partitioning of Eu2+ in plagioclase causes a negative Eu anomaly to develop in coexisting melts and clinopyroxene. In wet magmas, clinopyroxene crystallizes before plagioclase, and so initially appears with a negligible Eu anomaly. Clinopyroxenes then record water content in the delayed development of their negative Eu anomaly, caused by the delayed appearance of plagioclase along the cotectic with increasing water. We have tested this model using tephras from the 1723 eruption of Irazu, the ET3 unit of Arenal and the 1995 eruption of Cerro Negro volcanoes in Central America, with known water contents of $\sim$ 3, 4 and 5 wt%, respectively, based on olivine-hosted melt inclusions. Clinopyroxene phenocrysts separated from these samples vary in Mg\# from 86-72, and in some cases span the entire liquid line of descent of the volcano. REE patterns were determined by laser ablation ICPMS on 150 micron spots. A marked increase in the magnitude of the negative Eu anomaly occurs in clinopyroxenes with Mg\# $<$ 84 in Irazu, $<$ 82 in Arenal and $<$ 80 in Cerro Negro. These decreasing Mg\#'s correspond to decreasing liquidus temperatures at plagioclase saturation, in proportion to the known water contents of the magmas. Such systematics are broadly reproduced by predictions based on pMELTS, and experimental phase equilibria. This technique thus holds promise as a rapid method of determining the water content of virtually any arc volcanic rock, even those altered or ancient, with a resolution $<$ 0.5 wt% H2O.
DE: 3640 Igneous petrology
DE: 3670 Minor and trace element composition
DE: 1025 Composition of the mantle
DE: 1030 Geochemical cycles (0330)
SC: Volcanology, Geochemistry, Petrology [V]
MN: 2004 AGU Fall Meeting