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Isotopic equilibrium/disequilibrium in granites, metasedimentary rocks and migmatites (Damara orogen, Namibia) - a consequence of polymetamorphism and melting

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http://pubman.mpdl.mpg.de/cone/persons/resource/persons101043

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

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Jung, S. (2005). Isotopic equilibrium/disequilibrium in granites, metasedimentary rocks and migmatites (Damara orogen, Namibia) - a consequence of polymetamorphism and melting. Lithos, 84(3-4), 168-184.


Cite as: http://hdl.handle.net/11858/00-001M-0000-0014-8A94-9
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