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Geochemie und Geochronologie des Erongo-Komplexes, Namibia

Authors

Wigand,  Marcus Oliver
Scientific Technical Report STR, Deutsches GeoForschungsZentrum;
4.2 Inorganic and Isotope Geochemistry, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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0502.pdf
(Publisher version), 20MB

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Citation

Wigand, M. O. (2005): Geochemie und Geochronologie des Erongo-Komplexes, Namibia, PhD Thesis, (Scientific Technical Report STR ; 05/02), Potsdam : GeoForschungsZentrum, 99 p.
https://doi.org/10.2312/GFZ.b103-050283


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_8662
Abstract
The Erongo complex is the largest of the Cretaceous igneous complexes in the Damaraland, Southern Etendeka Province, Namibia. Erongo is made up of a series of mainly silicic volcanic and intrusive units, like many of the Damaraland complexes, but it is unique by virtue of its size and well-preserved igneous sequence silicic magmas as well as tholeiitic and alkaline basalts.The goals of this study were to determine the ages and petrogenetic relationships of the silicic and basic units in the Erongo complex, and to contribute to understanding the magmatic evolution of the Damaraland province. As part of this investigation, Os isotope compositions were determined on basic rocks from the complex, and this is the first study of Os isotopes in the Etendeka Province.