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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;

/persons/resource/persons101140

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