Classification of gem deposits of Sri Lanka

  • C.B. Dissanayake Institute of Fundamental Studies, Hantana Road, Kandy, Sri Lanka
  • M.S. Rupasinghe Institute of Fundamental Studies, Hantana Road, Kandy, Sri Lanka
Keywords: placer deposits, pegmatites, origin of gems

Abstract

Approximately 25% of Sri Lanka's landmass is gem-bearing. Most of the gem deposits are located in restricted zones (approximately 15000 sq km) within the area occupied by rocks of the Highland/Southwestern Complex . Over 90% of Sri Lanka's gem mining is from secondary placer deposits that can be classified as sedimentary gem deposits of residual, eluvial and alluvial types. Primary or in-situ gem occurrences are located mainly in contact-metamorphic zones comprising of skarn and calcium-rich rocks. Corundum occurrences have also been found in aluminous-rich, silica-deficient metasedimentary formations. Gem minerals that are frequently found in pegmatites within the Highland/Southwestern Complex include corundum, zircon, beryl, quartz varieties, feldspar and chrysoberyl. A special feature of many secondary gem deposits of Sri Lanka is their location on morphotectonically controlled sites.

Published
1995-01-01
How to Cite
C.B. Dissanayake, & M.S. Rupasinghe. (1995). Classification of gem deposits of Sri Lanka. Netherlands Journal of Geosciences, 74, 79-88. https://doi.org/10.70712/njg.v74.12406
Section
Regular paper