1000 resultados para Ba al Zion
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Dwd Ben-Gern Dai
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... neettq li-len akenaz ... "y ... ank miq-q"q Frankfur Ben-Hir
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le-... Yn Grnd
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Mit handschriftlichen Anmerkungen
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The barium distribution in sediments and pore fluids from five sites drilled in the Japan Sea have been used to illustrate the geochemical behavior of this element as it pertains paleoproductivity reconstructions, diagenetic remobilization, and barite precipitation in authigenic fronts. Sites where sulfate is depleted in the pore fluids also show high concentrations of dissolved barium, reflecting dissolution of biogenic barite. The high rate of sedimentation at Sites 798 and 799 results in a rapid sulfate depletion, which in turn leads to barite dissolution and reprecipitation in diagenetic fronts. The dissolved barium distribution at these sites has been used to quantify the rate of barite dissolution; we estimate a first-order rate constant for barite dissolution to be 2*10**-6/s at Site 799 and 2*10**-7/s at Site 798. Authigenic barite has been documented in sediments from Site 799 at 323 meters below seafloor by scanning electron microscopy and X-ray fluorescence analysis. These results indicate barite precipitation in a diagenetic front near the zone of sulfate depletion by upward migration of dissolved barium and downward diffusion of sulfate. Barite precipitation has also been inferred at Sites 796 and 798 based on sedimentary and dissolved barium distributions. Sulfate is not depleted in the pore fluids of Site 794. The lack of diagenetic remobilization of biogenic barium at this site preserves the high barium signal associated with the high-productivity sequences deposited during the late Miocene to Pliocene. Significantly, the organic carbon distribution does not indicate high accumulation rates during the periods of high opal and barium deposition. Instead, higher organic carbon accumulations are recorded in the Quaternary and middle Miocene sequences; intervals that are also characterized by deposition of siliciclastic turbidites. The presence of a terrestrial component in the organic carbon record renders barium a more useful indicator than organic carbon for paleoproductivity reconstructions in this marginal sea.
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[Mamd ibn Muammad].
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lil-Shaykh Fat Allh ibn al-Shaykh Sayyid Ab Bakr al-Bannn.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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Includes bibliographical references.
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A Teologia de Sio expressa pela tradio dos filhos de Cor de certa forma curiosa. implicante admitir a idia de uma influncia cananeia na Teologia de Sio. No h como negar esse fato, pois o Salmo 48 parece realmente possuir esta influncia. uma influncia cananeia e tambm das tradies do Sul judata. Esta pesquisa tem por objetivo analisar tal teologia de Sio existente em Jerusalm e apresentada no Salmo 48. Isto para chegar a uma resposta acerca da influncia que os filhos de Cor podem ter sofrido da religio cananeia, ao utilizar elementos dos mitos cananeus na composio do Salmo 48 e de outros salmos de sua coleo. Termos como Safon, mar, morte, Monte Sio e outros, e conceitos como mitologia, montanha sagrada, extremidade do mundo, Olimpo, etc, fazem pensar que eles de fato queriam sobrepor os mitos cananeus apresentando uma nova leitura, a partir da f em Jav. Os filhos de Cor possuam tradio do Norte israelita. As cidades onde eles habitaram estavam situadas em Efraim, Manasss e D. Algumas cidades de Manasss e Efraim eram cananeias. Os reis do Norte eram em sua maioria promotores da religio cananeia. Este era o ambiente onde os filhos de Cor habitaram e cumpriram seu ministrio levtico.
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Microfilm.
