Geology and geochemistry of the Barby formation, Sinclair Sequence: Progress Report for 1982/1983
The Sinclair Sequence is situated in South West Africa approximately 100 km south-west of Maltahöhe. The rocks are dominantly igneous in origin and comprise both extrusive and intrusive varieties. The present study is primarily concerned with the volcanic rocks of the Barby Formation.
Communications of the Geological Survey of South West Africa/Namibia
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Geology and geochemistry of the Barby formation_Sinclair Sequence.pdf | 333.41 KB |