986 resultados para 6-coordinate Copper(ii)
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Manganese nodules made of radiating rods of well crystallized birnessite were sampled at 8 degree 481.2'N, 103 degree 53.8W, 1875 m below sea level by a dredge that also collected hyaloclastite and basaltic talus. The nodule field is on the floor of a caldera within a young tholeiitic seamount and was discovered and photographed during a deep-two survey. It is interpreted as a brecciated hydrothermal deposit, crystallized from an amorphous manganese oxide precipitate that formed when seawater-based hydrothermal fluids mixed with oxidized seawater. The nodules and surrounding igneous rocks have subsequently been encrusted with hydrogenous ferromanganese oxides.
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Fluid inclusions in variably altered diabase recovered from Ocean Drilling Program Legs 137 and 140 at Hole 504B, Costa Rica Rift, exhibit fluid salinities up to 3.7 times that of seawater values (11.7 wt% NaCl equivalent) and exhibit uncorrected homogenization temperatures of 125°C to 202°C. The liquid-dominated inclusions commonly are entrapped in zones of secondary plagioclase and may be primary in origin. Fluid salinities are similar to compositions of fluids venting on the seafloor (0.4-7.0 wt% NaCl) and overlap with those measured in metabasalt samples recovered from near the Kane Fracture Zone on the Mid-Atlantic Ridge and from the Troodos ophiolite, Cyprus. The salinity variations may reflect hydration reactions involving formation of secondary mineral assemblages under rock-dominated conditions, which modify the ionic strength of hydrothermal fluids by consuming or liberating water and chloride ion. Rare CO2-CH4-bearing inclusions, subjacent to zones where talc after olivine becomes an important secondary mineral phase (1700 mbsf), may have formed due to local interaction of seawater and olivine at low water to rock ratios. Corrected average fluid inclusion homogenization temperatures exhibit a gradient from 159°C at a depth of 1370 mbsf to 183°C at a depth of 1992 mbsf and are in apparent equilibrium with the present conductive downhole temperatures. These data indicate that fluid inclusions may be used to estimate downhole temperatures if logging data are unavailable. The compositional and thermal evolution of the diabase-hosted fluids may reflect late-stage, off-axis circulation and conductive heating of compositionally modified seawater in the sheeted dike complex at Hole 504B.
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CCPB000219746-4 (t. III)
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Pie de imp. T. IV: Imprenta de R. Campuzano.
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Mode of access: Internet.
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Las iniciales A. B. corresponden a Alejandro de Bacardí y de Janer.
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Mode of access: Internet.
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Vols. 16-20 have engravings in two states, satin and paper.
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Text in Greek; introd. and notes in Latin.
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Available on demand as hard copy or computer file from Cornell University Library.
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12. Bd. Vermischte schriften: Einleitung zu "Kahldorf über den adel." Vorrede zum ersten bande des "Salon." Ueber den denuncianten. Der Schwabenspiegel. Einleitung zur prachtausgabe des "Don Quixote." Vorwort zu A. Weill's "Sittengemälden aus dem elsässichen volksleben." Thomas Reynolds. Ludwig Marcus. Loeve-Veimars. Autobiographische skizze. Albert Methfessel. Die romantik. Vershiedenartige geschichtsauffassung. Eingangswort zur uebersetzung eines lappländischen gedichts. Recensionen. Nachträge. Gedanken und einfälle.
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Contiene : Tomo I (XXX,336,[6] p.). - Tomo II (352,[4] p.). - Tomo III (332,[3] p.). -Tomo IV (366,[6] p.). - Tomo V (369,[3] p.). - Tomo VI (354,[6] p.)
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T. IV incluye Nomenclatura biográfica de los principales teólogos y de sus obras teológicas desde S. Juan Damasceno hasta nuestros días (p.549-586)
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I. CLIII, 206 p. pl. 1-12 (col.) 1823. II. abt. 1. 182[6] p. 1827. II. abt. 2. 208 p. pl. 13-43 (col.) 1831.