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Photomicrography > Corundum > Metamorphic rubies & sapphires
First draft: May 15th, 2014 | Last update: June 14th, 2016
Some Features Observed in Metamorphic Rubies & Sapphires
Greenland, Mozambique, southern Madagascar,
Myanmar (Burma), Sri Lanka (Ceylon), Tanzania & northern Vietnam
Metamorphism is a geological process in which pre-existing or parent rocks recrystallise following changes either in temperature and pressure or by rock-fluid interaction (metasomatism). Fluids usually contain chemicals that may mobilise other elements to participate in the recrystallisation process.
The main geological processes triggering parent rock recrystallisation and injection of fluids include tectonic activity and magmatic intrusions, implying that parent rocks may even melt prior to recrystallisation - a process called anatexis. The latter lays a foundation for the formation of magmatic corundum.
The basic requirement for corundum formation is a parent rock rich in aluminium, Al, depleted of or poor in silicon, Si, and containing the necessary chromophores. Consequently, a wide variety of rocks are candidates, while intrusions or fluids may facilitate further depletion of Si: desilicification.
Subjected to metamorphic Amphibolite facies (650°C; 4.5-6.5 kbar) or Granulite facies (700-750°C; 8-10.5 kbar) conditions, Nature created gems from the parent rocks' mineral assemblages with a geochemistry and inclusion scene that is completely different from rubies and sapphires of magmatic origin.
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