980 resultados para 63-20 µm gU


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Vorbesitzer: Abraham Merzbacher

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Vorbesitzer: Johannes Latomus; Bartholomaeusstift Frankfurt am Main

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Vorbesitzer: Johann Hartmann Beyer

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Vorbesitzer: Freiherrlich Carl von Rothschild'sche Bibliothek Frankfurt am Main (Bibliothek für Neuere Sprachen und Musik)

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Sand-silt-clay distribution was determined at Scripps on samples collected at the time the cores were split and described. The sediment classification used here is that of Shepard (1954); sand, silt, and clay boundaries are determined on the basis of the Wentworth (1922) scale. Thus the sand, silt, and clay fractions are composed of particles whose diameters range from 2000 to 62.5 µm, 62.5 to 3.91 µm, and less than 3.91 µm, respectively. This classification is applied regardless of sediment type and origin.

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This paper discusses the distribution of clay minerals and identification of their assemblages in relation to sedimentary facies encountered during DSDP Leg 63 drilling off southern California and Baja California. We also consider how these assemblages are determined by source areas and changes in general paleogeographic environments during different periods of sedimentation.