Petrogenesis of the Mesoproterozoic anorthosite, syenite and carbonatite suites of NW Namibia and their contribution to the metasomatic formation of the Swartbooisdrif sodalite deposits
During the Mesoproterozoic large volumes of magma were repeatedly emplaced within the basement of NW Namibia. Magmatic activity started with the intrusion of the anorthositic rocks of the Kunene Intrusive Complex (KIC) at 1,385-1,347 Ma. At its south-eastern margin the KIC was invaded by syenite dyk...
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https://opus.bibliothek.uni-wuerzburg.de/frontdoor/index/index/docId/600http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-6987
https://nbn-resolving.org/urn:nbn:de:bvb:20-opus-6987
https://opus.bibliothek.uni-wuerzburg.de/files/600/Appendix.pdf
https://opus.bibliothek.uni-wuerzburg.de/files/600/Dissertation.pdf
https://opus.bibliothek.uni-wuerzburg.de/files/600/Plate_1.pdf
https://opus.bibliothek.uni-wuerzburg.de/files/600/Plate_2.pdf
https://opus.bibliothek.uni-wuerzburg.de/files/600/Plate_3.pdf
https://opus.bibliothek.uni-wuerzburg.de/files/600/Plate_4.pdf