Die Hypothesen der Bibelkritik und der Commentar zur Genesis von Herrn Rabbiner S. R. Hirsch

Joseph Gugenheimer

Die Hypothesen der Bibelkritik und der Commentar zur Genesis von Herrn Rabbiner S. R. Hirsch

Joseph Gugenheimer

die Hypothesen der Bibelkritik und der Commentar zur Genesis von Herrn Rabbiner S. R. Hirsch

Joseph Gugenheimer

Ms. Barth. 34 - Liber Genesis et Exodi cum glossa ordinaria

Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Die hebräische Genesis

Digitalisat enth.: Teil 1.Texte; Teil 2. Zur Quellenscheidung u. Textkritik

Zur Genesis der afrikanischen Flora

Von Prof. Dr. J. Palacký

Die Genesis des Judenthums

von Karl Christian Wolf

Die Genesis

historisch-kritisch erläutert von P. von Bohlen

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1423 - Genesis des Systems

Bereitgestellt mit freundlicher Unterstützung der Staatsbibliothek zu Berlin - Preußischer Kulturbesitz

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1424 - Genesis des Systems

Bereitgestellt mit freundlicher Unterstützung der Staatsbibliothek zu Berlin - Preußischer Kulturbesitz

Eden und seine Umgebung : Rede über Genesis 2, 10 ; gehalten bei der Trauung seiner innigstgeliebten Kinder, Dr. med. Sigmund Theodor Stein und Eugenie Thekla, geb. Levi, im Betsaal der Westend-Union zu Frankfurt am Main, Dienstag, den 5. Mai 1874

von Leopold Stein

The influence of contact pressure, moisture, and compression time on the performance of cotton anti-contamination clothing

The objectives of this research were (1) to study the effect of contact pressure, compression time, and liquid (moisture content of the fabric) on the transfer by sliding contact of non-fixed surface contamination to protective clothing constructed from uncoated, woven fabrics, (2) to study the effect of contact pressure, compression time, and liquid content on the subsequent penetration through the fabric, and (3) to determine if varying the type of contaminant changes the effect of contact pressure, compression time, and liquid content on the transfer by sliding contact and penetration of non-fixed surface contamination. ^ It was found that the combined influence of the liquid (moisture content of the fabric), load (contact pressure), compression time, and their interactions significantly influenced the penetration of all three test agents, sucrose- 14C, triolein-3H, and starch-14C through 100% cotton fabric. The combined influence of the statistically significant main effects and their interactions increased the penetration of triolein- 3H by 32,548%, sucrose-14C by 7,006%, and starch- 14C by 1,900%. ^

Geological and geochemical characteristics of the Tersang gold deposit, Malaysia: implications for genesis and gold exploration

The Central gold belt of peninsular Malaysia comprises a number of gold deposits located in the east of the N-S striking Bentong-Raub Suture Zone. The Tersang gold deposit is one of the gold deposits in the gold belt and hosted in sandstone, rhyolite and breccia units. The deposit has an inferred resource of 528,000 ounces of gold. The geochronology of the Tersang deposit has been newly constrained by LA ICP-MS U-Pb zircon dating. The maximum depositional age of the host sedimentary rocks ranges from Early Carboniferous to Early Permian (261.5 ± 4.9 Ma to 333.5 ± 2.5 Ma) for the host sandstone and Late Triassic for the rhyolite intrusion (218.8 ± 1.7 Ma). Textural characteristics of pyrite have revealed five types including (1) Euhedral to subhedral pyrite with internal fracturing and porous cores located in the sandstone layers (pyrite 1); (2) Anhedral pyrite overgrowths on pyrite 1 and disseminated in stage 1 vein (pyrite 2); (3) Fracture-filled or vein pyrite located in stages 1 and 2 vein (pyrite 3); (4) Euhedral pyrite with internal fractures also located in stage 2 vein (pyrite 4); and (5) Subhedral clean pyrite located in the rhyolite intrusion (pyrite 5). Based on pyrite mapping and spot analyses, two main stages of gold enrichment are documented from the Tersang gold deposit. Gold in sandstone-hosted pyrite 1 (mean 4.3 ppm) shows best correlation with Bi and Pb (as evidenced on pyrite maps). In addition, gold in pyrite 3 (mean 8 ppm) located in stage 2 vein shows a good correlation with As, Ag, Sb, Cu, Tl, and Pb. In terms of gold exploration, we suggest that elements such as As, Ag, Sb, Cu, Tl, Bi, and Pb associated with Au may serve as vectoring tools in gold exploration. Our new geological, structural, geochemical and isotopic data together with mineral paragenesis, pyrite chemistry and ore fluid characteristics indicate that the Tersang gold deposit is comparable to a sediment-hosted gold deposit. Our new genetic model suggests deposition of the Permo-Carboniferous sediments followed by intrusion of rhyolitic magma in the Late Triassic. At a later stage, gold mineralisation overprinted the rhyolite intrusion and the sandstone.