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Science 27 October 1995: Vol. 270. no. 5236, pp. 625 - 627 DOI: 10.1126/science.270.5236.625
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Reports
Cross-Arc Geochemical Variations in the Kurile Arc as a
Function of Slab Depth
Jeffrey G. Ryan (1),
Julie Morris (2),
Fouad Tera,
William P. Leeman,
Andrei Tsvetkov
Lavas from transects across the Kurile Islands arc showed
geochemical variations related to changes in the compositions of fluids
derived from the subducting slab. Enrichment factors for boron, cesium,
arsenic, and antimony, all elements with strong affinities for water,
decreased across the arc. This decrease is presumably related to losses
of water-rich fluids during the dehydration of the subducting plate.
Enrichments of potassium, barium, beryllium-10, and the light rare
earth elements remained constant; these species may move in silica-rich
fluids liberated from the slab at greater depths.
J. G. Ryan, Department of Geology, University of South Florida,
Tampa, FL 33620, USA, and Department of Terrestrial Magnetism, Carnegie
Institution of Washington, Washington, DC 20015, USA.
J. Morris and F. Tera, Department of Terrestrial Magnetism, Carnegie
Institution Washington, Washington, DC 20015, USA.
W. P. Leeman, Department of Geology and Geophysics, Rice University,
Houston, TX, USA.
A. Tsvetkov, Institute of Mining and Mineral Resources, Russian Academy
of Sciences, Moscow, Russia.
(1) To whom correspondence should be addressed.
(2) Present address: Department of Earth and Planetary Sciences,
Washington University, St. Louis, MO, USA.
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