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Geochemistry of granite in-situ low-melt fractions : an example from the Central Damara Orogen / S. Jung; E. Hoffer; P. Masberg; S. Hoernes

By: Contributor(s): Material type: TextTextLanguage: English Series: Communications of the Geological Survey of Namibia, Volume 10, 1995, p. 21-31Publication details: Windhoek : Geological Survey of Namibia, 1995,: Multi ServicesEdition: Special issue: Proterozoic crustal and metallogenic evolutionDescription: 11 pages : fig., tables; 30 cmISSN:
  • 0256-1697
Subject(s): DDC classification:
  • PER 553 Communications of the Geological Survey of Namibia
Summary: This paper discusses several phenomena of in-situ migmatization in connection with intrusion of peraluminous granites which were generated in the lower crust and intruded inhigh-grade metasediments to form vein-like migmatites. The migmatitic complex studied is located in the Omaruru River in the central Damara Orogen, Namibia consists mainly of migmatites generated by intrusion of granites. The studied granites are syntectonic, medium- to fine-graidut leucogranites
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This paper discusses several phenomena of in-situ migmatization in connection with intrusion of peraluminous granites which were generated in the lower crust and intruded inhigh-grade metasediments to form vein-like migmatites. The migmatitic complex studied is located in the Omaruru River in the central Damara Orogen, Namibia consists mainly of migmatites generated by intrusion of granites. The studied granites are syntectonic, medium- to fine-graidut leucogranites

Geological Survey of Namibia Serie

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