(Mererani)
Gem mining area 70 km from Arusha, where tanzanite was first found in 1968.
The occurrence of gem-quality tanzanite and grossular has been found to occur mainly in boudinaged pegmatitic veins and hydrothermal fracture fillings. These fracture fillings occur in brecciated and hydrothermally altered graphite-bearing gneiss in a mineral association containing glass-clear quartz, diopside, zoisite, graphite and calcite.
Refs.:
- Barot, N.R. and Boehm, E.W. (1992) Gem Quality Green Zoisite, Gems & Gemology: Spring 1992: 28(1).
- http://www.ajol.info/viewarticle.php?id=16567&jid=98&layout=abstract