Single-zircon U-Pb dating of Carboniferous-Permian tuffs, Namibia, and the intercontinental deglaciation cycle framework
The Carboniferous-Permian Dwyka Group in southern Namibia is subdivided into four upward-fining deglaciation sequences, each of which is capped by finegrained glaciolacustrine or glaciomarine deposits. Both the second and the third deglaciation sequences
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|Source:||Geological Society of America. Special Papers|
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