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  • 1980-1984  (3)
Material
Years
Year
  • 1
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of physical chemistry 〈Washington, DC〉 87 (1983), S. 1464-1466 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    New York : Cambridge University Press
    Victorian literature and culture 11 (1983), S. 127-148 
    ISSN: 1060-1503
    Source: Cambridge Journals Digital Archives
    Topics: English, American Studies , History
    Notes: The poet – speaker of Book 1 of The Ring and the Book believed that the first two monologues of his grand poem balanced one another. In his preview of the monologues, he writes that Half-Rome and Other Half-Rome are equally unsuccessful in their efforts to find the truth of the murder story. The speakers possess an “opposite feel” for the truth, but each achieves a “like swerve, like unsuccess” (I.883–84). Although Other Half-Rome succeeds in being on the right side of the issue, Browning as poet-speaker considers his defense of Pompilia to be the result only of luck or a “fancy-fit.” This “fancy-fit” is a mood which inclines the speaker to choose Pompilia as it might incline him to choose between two runners in a race according to the colors of their scarves (1.885–92). Browning sets this speech by a Bernini fountain, one where Triton blows water through a conch: “Puffs up steel sleet which breaks to diamond dust” (1.900). The poet may have intended this setting to suggest the way in which he views the language and imagery that Other Half-Rome uses to tell his story. The speaker's mixture of Christian and classical mythology and his concern for the painterly qualities of Pompilia's deathbed scene do suggest an aesthetic temperament. The poet may have considered the speech of such a man to be “diamond dust” signifying nothing. In any case, the poet-speaker of Book 1 concludes his description of Other Half-Rome by saying, with apparent sarcasm, that to this speaker Pompilia “seemed a saint and martyr both” (1.909). This assessment of Other Half-Rome has been the subject of disagreement among commentators on the poem.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 81 (1982), S. 277-289 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The occurrence and origin of marialitic scapolite in the Humboldt lopolith was investigated in the field and in the laboratory using petrographic and experimental techniques. Scapolite occurs in three modes: as a pervasive replacement of plagioclase and other minerals in gabbro, diorite and extrusive rocks; as a poikiloblastic mineral in scapolitite dikes; and as a fracture-filling mineral with analcime, albite and sphene in scapolite veins. Additional secondary minerals associated with scapolite include epidote, prehnite, hornblende and diopside-salite clinopyroxene. Relations with these minerals suggest that most marialitic scapolite grew at temperatures around 400° C. Scapolite composition varies from EqAn12 to EqAn37, containing from 72 to 96 atomic% Cl in the R position. Experiments on systems of similar compositions indicate that NaCl-H2O fluid having more than 40 mol% NaCl is needed to stabilize the scapolite. Variation in scapolite compositions is due to thermal and fluid compositional gradients normal to conduits of hydrothermal fluids, and occurs on a scale up to 100 m. The likely source of Na and Cl is pre-existing evaporites or evaporitic brine derived from the wallrocks. Salinity could have been increased to a level sufficient to stabilize scapolite by hydration of an originally dry magma, possibly aided by hydrothermal boiling. Results may be applied to hydrothermal alteration in areas of rifting or back-arc spreading, and in mid-ocean ridge hydrothermal systems.
    Type of Medium: Electronic Resource
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