Trace element and isotopic (Sr, Nd, Pb, O) arguments for a mid- to lower 
crustal origin of Pan-African garnet-bearing S-type granites from the Damara 
orogen (Namibia)

Jung, S.; Mezger, K.; Hoernes, S.

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Trace element and isotopic (Sr, Nd, Pb, O) arguments for a mid- to lower crustal origin of Pan-African garnet-bearing S-type granites from the Damara orogen (Namibia)

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Jung, S.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Mezger, K.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Jung, S., Mezger, K., & Hoernes, S. (2001). Trace element and isotopic (Sr, Nd, Pb, O) arguments for a mid- to lower crustal origin of Pan-African garnet-bearing S-type granites from the Damara orogen (Namibia). Precambrian Research, 110, 325-355.

Cite as: https://hdl.handle.net/11858/00-001M-0000-0014-940C-E

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