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Titlebook: Messung, Modellierung und Bewertung von Rechensystemen; 3. GI/NTG-Fachtagung Heinz Beilner Conference proceedings 1985 Springer-Verlag Berl

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O. Gihr,P. J. Kuehn2.7 m of compacted sediment per 10,000 years in the following way. The thickness of the Liesberg Member was measured to be 25 m at the type locality in the clay pit of Hinter Chestel south of Liesberg, in section RG 306, which is represented in . (2000a, Pl. 31). The Liesberg Member is part of the .
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Peter Paul Spies between the Callovian and the Oxfordian Stage in section RG 208 near Ueken in Canton Aargau are thin, but they are not stratigraphically condensed in this section. The beds are shown in Figs. 4.14 and 8.2. A diverse ammonite assemblage of almost 10,000 specimens was recently collected from . out of
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H. Kramer,J. Gorissending plane of bed no.17 of section RG 434 that he measured in July of 1986 in the eastern quarry of Steingrueben on the territory of the township of Oberdorf, northwest of the city of Solothurn (. 2000a, Pl. 42, and . 2003, p. 156). The very distinct footprints had a diameter of 0.5 and 0.7 m, respe
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H. Beilner,H. Scholtennerated tables of representative square roots of –1 are given for all Clifford algebras with . = 5,7, and . = 3 (mod 4) with the associated ring ℂ. This includes, ., .. important in Clifford analysis, and .. which in applications is at the foundation of conformal geometric algebra. All these roots o
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N. Haak,K. Kittmannnerated tables of representative square roots of –1 are given for all Clifford algebras with . = 5,7, and . = 3 (mod 4) with the associated ring ℂ. This includes, ., .. important in Clifford analysis, and .. which in applications is at the foundation of conformal geometric algebra. All these roots o
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