Full Text URL
https://doi.org/10.1126/science.270.5236.625
Article
Cross-Arc Geochemical Variations in the Kurile Island Arc as a Function of Slab Depth
Science
Document Type
Article
Publication Date
10-1-1995
Keywords
- Kurile Islands,
- Geochemistry
Digital Object Identifier (DOI)
https://doi.org/10.1126/science.270.5236.625
Disciplines
Abstract
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.
Citation / Publisher Attribution
Science, v. 270, issue 5236, p. 625-628
Citation Information
Jeffrey G. Ryan, Julie Morris, Fouad Tera, William P. Leeman, et al.. "Cross-Arc Geochemical Variations in the Kurile Island Arc as a Function of Slab Depth" Science Vol. 270 Iss. 5236 (1995) p. 625 - 627 Available at: http://works.bepress.com/jeffrey_ryan/46/