960 resultados para Glass painting and staining, French.
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Geochemical data from plagioclase-hosted silicate melt inclusions from Leg 140, Hole 504B diabase dikes are reported. Hand-picked plagioclase grains were heated to 1260°-1280°C to remelt the glass inclusions and to infer trapping temperatures. The samples were then polished to expose the inclusions, which were analyzed by electron and ion microprobes. Inclusion compositions are mainly in equilibrium with the host plagioclase and are more depleted in incompatible elements than the host rock. Simple crystal-liquid equilibrium calculations show that the melt inclusions could have been in equilibrium with depleted abyssal peridotite diopsides, whereas whole-rock basalt compositions generally could not have been. The melt inclusions are significantly more depleted than normal (N-type) mid-ocean-ridge basalt (MORB) and are consistent with being produced by 8%-16% incremental or open-system melting with 2% residual porosity in the peridotite source. These magmas were formed during pressure-release melting of the mantle over a range of depths between 30 and 15 km.
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"This 'Practical guide' is a reprint of the chapter on 'The Library of Congress' in the Washington standard guide"--Title-page verso.
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Includes index.
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Mode of access: Internet.
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Mode of access: Internet.
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The plates are mounted.
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"Copyright ... Boston public library employees benefit association."
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Latest issue consulted: Vol. 15 [i.e. v. 18] (summer 2004).
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Adapted in abbreviated form from the French edition, originally compiled and edited by P.J. Hetzel with many contributions by himself.
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With descriptive letterpress.
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"Sketches of persons who acted only in the revolution, or in that and the French war": p. 470-573.
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Bibliography: p. 243-245.
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Cover-title.
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