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

Lithos

Volumn 84, Issue 3-4, 2005, Pages 168-184

  Jung, S ^a,b  

^a MAX PLANCK INSTITUTE FOR CHEMISTRY   (Germany)

^b PHILIPPS UNIVERSITY MARBURG   (Germany)

Author keywords

A type granite; Damara orogen; Isotopes; S type granite

Indexed keywords

CRUSTAL RECYCLING; GRANITE; ISOTOPIC COMPOSITION; MELTING; METAMORPHISM; METASEDIMENTARY ROCK; MIGMATITE; OROGENIC BELT; XENOLITH;

AFRICA; DAMARA BELT; EASTERN HEMISPHERE; NAMIBIA; SOUTHERN AFRICA; SUB-SAHARAN AFRICA; WORLD;

EID: 25144453249     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2005.03.013     Document Type: Article

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