(Кемпирсай)
Giant podiform chromite deposit with reserves >300 Mt of Cr2O3. Presented as some tens of chromite pods and lenses on a 30x50 km territory. It is hosted by harzburgite and dunite rocks metamorphised at amphibolite facies conditions.
Located in the metasedimentary silurian Sakmara belt.
Refs.:
- Melcher F., Grum W., Simon G., Thalhmmer T. & Stumpfl E.F. (1997): Petrogenesis of the ophiolitic giant chromite deposits of Kempirsai, Kazakhstan: a study of solid and fluid inclusions in chromite. Journal of Petrology 38, 1419–1458.
- http://www.gl.rhul.ac.uk/geode/Uralides/Kempirsai.html