989 resultados para 173-1066
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abgedruckt in: Schopenhauer-Jahrbuch 39 (1958), S. 128-129 (Teilabdruck)
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Zu Stoltzes Besuch in Weinsberg
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19 Briefe zwischen Lisa Witherell (geb. Richter) und Max Horkheimer, 1963-1971; 2 Briefe zwischen Werner Wittayer (stud. phil.) und Max Horkheimer, 1964; 4 Drucksachen vom Landtagspräsidenten Otto Witte an Max Horkheimer, 1952-1954; 2 Briefe an Otto Witte von Max Horkheimer, 1952-1953; 1 Todesanzeige, 1963; 4 Briefe zwischen der Studentin Ulrike Wittenberg und Max Horkheimer, 1972-1973; 4 Briefe zwischen dem Professor Karl A. Wittfogel und Max Horkheimer, 1972; 3 Briefe zwischen dem Oberstudiendirektor Dr. Kurt Debus und Max Horkheimer, 1967; 3 Briefe zwischen David Wodlinger und Max Horkheimer, 1960; 2 Briefe zwischen Dr. Herman Wohlstein und Max Horkheimer, 1965; 16 Briefe an Johanna Woitschach von Max Horkheimer, 1970-1973 (die Briefe an Max Horkheimer wurden zurückverlangt); 1 Brief von Ernst Wolf an Max Horkheimer, San Francisco, 1954; 3 Briefe zwischen dem Diplom-Psychologen Heinz E. Wolf und Max Horkheimer, 1958; 13 Briefe zwischen dem Oberstudiendirektor Oskar Wolfenstädter und Max Horkheimer, 1968-1969; 4 Briefe zwischen der Ordensschwester Katherine Wolff und Max Horkheimer, 1970-1971; 25 Briefe zwischen Margo H. Wolff und Max Horkheimer, 1962-1973; 11 Briefe zwischen dem Professor Max Wolff und Max Horkheimer, 1960; 3 Briefe zwischen dem Professor Manfred Wolfson und Max Horkheimer, 1971; 6 Briefe von der Physiotherapeutin Helga Wolk an Max Horkheimer, 1970-1971; 13 Briefe zwischen Hedwig G. de Wollenberger und Max Horkheimer, 1966-1970; 1 Brief an den Professor Günther Wollheim von Max Horkheimer, 1965; 4 Briefe zwischen Johanna Wopperer-Ege und Max Horkheimer, 1970; 5 Briefe zwischen Anton Wopperer und Max Horkheimer, 1969-1970; 3 Briefe an die World Future Society von Max Horkheimer, 1969-1973; 2 Briefe zwischen dem World Jewish Congress und Max Horkheimer, 1970; 2 Briefe zwischen dem Professor Theodor Würtenberger und Max Horkheimer, 1964; 3 Briefe zwischen der Würtembergischen Landesbibliothek und Max Horkheimer, 1969; 16 Briefe zwischen Rösle Wüstholz und Max Horkheimer, 1951-1959; 2 Briefe zwischen Christoph Wulf und Max Horkheimer, 1973; 1 Brief an Jssy Wygoda von Max Horkheimer, 1964; 2 Briefe zwischen Dr. Hans von Wyl und Max Horkheimer, 1971; 2 Briefe zwischen Jacques Wyler und Max Horkheimer, 1973; 1 Brief von Gisela Wysocki an Max Horkheimer, o.J. (1973?);
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Tochilinite (approximately FeS(Mg,Fe)(OH)2) is locally abundant in Hole 1068A serpentinites from Cores 173-1068A-21R and 22R. It occurs in veins, as fillings in void space, and in intergrowths with serpentine and andradite. An apparently related mineral, but with Ca and Al largely replacing Mg, occurs in association with, and possibly as a replacement of, pyrrhotite in serpentinite breccias from the bottom of Core 173-1068A-20R. The transition from Mg-Fe-rich brucite tochilinites to Ca- and S-rich carbonate tochilinites is consistent with increasing sulfur and oxygen activity upsection. Tochilinite has been reported at other sites on the Iberia Abyssal Plain and is abundant to the point of being a rock-forming mineral in several samples from Site 1068. Rather than being a mineralogical curiosity, tochilinite appears to be common and a major sink for sulfur in the upper serpentinites of the Iberia Abyssal Plain.
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Fil: Pró, Diego F..
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Mean values of radiogenic heat production are derived from measurements of radioelements on the following rock types: amphibolite (0.358 ± 0.118 µW/m**3) and tonalite gneiss (0.802 ± 0.039 µW/m**3) at Site 1067 and serpentinized peridotite (0.0108 ± 0.0003 µW/m**3) at Site 1068. The results for serpentinized peridotite and amphibolite are consistent with previous measurements on samples from Sites 897 and 900. These results suggest that the thin continental crust in this region would contribute very little to the conductive heat flow.
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Planktonic foraminifers recovered from five sites drilled off western Portugal during Ocean Drilling Program Leg 173 are documented. Hole 1065A yielded planktonic foraminifers from Miocene sediments in Sections 173-1065A-1R-1 through 6R-2. Hole 1067A penetrated middle Eocene sediments containing planktonic foraminifers in Section 173-1067A-1R-1 through Lower Eocene planktonic foraminiferal horizons to Section 12R-CC. Hole 1068A yielded planktonic foraminiferal assemblages from middle Eocene sediments at Section 173-1068A-1R-1 to Maastrichtian sediments at Section 173-1068A-15R-3, whereas Hole 1069A contained middle Eocene taxa in Section 173-1069A-1R-1 through Campanian/Maastrichtian forms in Section 173-1069A-15R-2. All of the planktonic foraminifers recovered from these sites are of poor to moderately good preservation and are variable in abundance. Hole 1070A yielded only six planktonic foraminifers, with the assemblages being dominated by benthic foraminifers and fish teeth. The co-occurrence of other microfossil groups, including benthic foraminifers, are only briefly discussed here. The lower Miocene biosiliceous facies recorded in Hole 1065A is considered to be coeval with a similar facies found in onshore sections farther to the east, in southern Spain.
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Fil: Blake, Cristina. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación. Instituto de Investigaciones en Humanidades y Ciencias Sociales (UNLP-CONICET); Argentina.
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Fil: Rogers, Geraldine. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
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Fil: Rogers, Geraldine. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.