Geologische Untersuchungen im Bereich der Damara-Sequenz und geochemische Analysen von Proben junger fluviatiler Sedimente, Blatt 1813 CD Tomakas, Kaokoveld, Namibia select="/dri:document/dri:meta/dri:pageMeta/dri:metadata[@element='title']/node()"/>

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dc.contributor.advisor Brey en_US
dc.contributor.advisor Kowalczyk en_US
dc.contributor.author Aurich Elke en_US
dc.date.accessioned 2013-07-02T14:10:35Z
dc.date.available 2013-07-02T14:10:35Z
dc.date.issued 2000 en_US
dc.identifier.uri http://hdl.handle.net/11070.1/4381
dc.description Includes bibliographical references en_US
dc.description.abstract English abstract provided by author: en_US
dc.description.abstract The following thesis " Geological study of the Damara Sequence and geochemical analysis of young fluvial sediments, sheet 1813 CD Tomakas, Kaokoveld, Namibia " is the result of a co-operation with the Geological Survey of Namibia. It is organized in two subdivisions: part A and part B. Task of part A (explanatory notes geological map) coros [sic] description of the observed rock formations of the pan-African Damara Sequence with regard to petrographic and structural-geological aspects and the correlation on the stratigraphic findings with those of former studies. Part B deals with mineral exploration on sheet 1813 CD of the Tomakas area. Furthermore according to the geochemical analysis (XRF) an overall statement of the distribution of elements and the resulting anomalies will be made (sheet 1813 CD Tomakas) en_US
dc.format.extent 110 p en_US
dc.format.extent ill en_US
dc.language.iso eng en_US
dc.subject Geology en_US
dc.title Geologische Untersuchungen im Bereich der Damara-Sequenz und geochemische Analysen von Proben junger fluviatiler Sedimente, Blatt 1813 CD Tomakas, Kaokoveld, Namibia en_US
dc.type thesis en_US
dc.identifier.isis F004-199299999999999 en_US
dc.description.degree Frankfurt en_US
dc.description.degree Germany en_US
dc.description.degree Johan Wolfgang Goethe University en_US
dc.description.degree Diplomarbeit en_US
dc.masterFileNumber 2700 en_US


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