973 resultados para 182-1130


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Felix Stössinger

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u.a.: Universität Halle; Hotel Englischer Hof; unglückliche Liebschaft, Krankheit; Gubnemaux; Brunner; Martin Emden;

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Vorbesitzer: Dominikanerkloster Frankfurt am Main

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Georg Pingler, Keine Gelegenheit, Stoltzes Gesuch beim Großherzog vorzubringen

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Fragebögen zur Studie, als Typoskript vervielfältigt, mit handschriftlichen Eintragungen, 1 Ordern; Dankesbrief an das Institut für Sozialforschung auf Grund der Zusendung des Forschungsberichts, von : Anders, Marga; Außenhandelnsjahrbuch; Bäuerle, Theodor; Belgien, Botschafter in Rom; Berlin, Bezirksamt Reinikenhof; Bernhard, Henry; Bernhard, Siegfried; Borsing A.G.; Heckel, Theodor; Hochschule für Politische Wissenschaft, München; Nordwestdeutscher Rundfunkt, Hamburg; Universität Hamburg, Philosophisches Seminar; Westfälische Rundschau; Stuttgart, Oberbürgermeister; Hessischer Rundfunk; Brief mit Unterschrift, 16 Blatt;

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Vorbesitzer: Johannes Peulen

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Detrital modes for 524 deep-marine sand and sandstone samples recovered on circum-Pacific, Caribbean, and Mediterranean legs of the Deep Sea Drilling Project and the Ocean Drilling Program form the basis for an actualistic model for arc-related provenance. This model refines the Dickinson and Suczek (1979) and Dickinson and others (1983) models and can be used to interpret the provenance/tectonic history of ancient arc-related sedimentary sequences. Four provenance groups are defined using QFL, QmKP, LmLvLs, and LvfLvmiLvl ternary plots of site means: (1) intraoceanic arc and remnant arc, (2) continental arc, (3) triple junction, and (4) strike-slip-continental arc. Intraoceanic- and remnant-arc sands are poor in quartz (mean QFL%Q < 5) and rich in lithics (QFL%L > 75); they are predominantly composed of plagioclase feldspar and volcanic lithic fragments. Continental-arc sand can be more quartzofeldspathic than the intraoceanic- and remnant-arc sand (mean QFL%Q values as much as 10, mean QFL%F values as much as 65, and mean QmKP%Qm as much as 20) and has more variable lithic populations, with minor metamorphic and sedimentary components. The triple-junction and strike-slip-continental groups compositionally overlap; both are more quartzofeldspathic than the other groups and show highly variable lithic proportions, but the strike-slip-continental group is more quartzose. Modal compositions of the triple junction group roughly correlate with the QFL transitional-arc field of Dickinson and others (1983), whereas the strike-slip-continental group approximately correlates with their dissected-arc field.

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Fil: Duarte Rust, Leandro. Universidade Federal do Mato Grosso (Brasil)