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|   Formula  | MgCO3            |  
 |  |   Optic class & sign  | Uniaxial negative |  
 |  |   Relief  | Low negative to high positive; sections with c at a low angle to the thin section plane show a marked change of relief over a 90° rotation; pronounced chagrin in high-relief position (= polarizer parallel to long diagonal of rhomb).            |  
 |  |   Refractive indices  | no = 1.700            
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ne = 1.509            
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| n and Δn data for endmember composition; n increases with substitution of Fe or Mn for Mg; n decreases with substitution of Ca for Mg            |  
 |  |   Birefringence   (max.) | 0.191            |  
 |  |     | Δn increases with substitution of Fe or Mn for Mg; Δn decreases with substitution of Ca for Mg            |  
 |  |   Sign of elongation  | Hardly applicable due to very high Δn            |  
 |  |   Interference figure  | Well-defined isogyre cross, isochromes over multiple colour orders            |  
 |  |   Colour /   pleochroism  | Colourless            |  
 |  |   Zoning  |    |  
 |  
 
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|   Form |   Habit  | Granular, also fibrous aggregates          |  
 |  |  |   Surface  | Anhedral, rarely euhedral            |  
 |  |   Cleavage  | 3 sets, rhombohedral {1011}, perfect            |  
 |  |   Twinning  | Generally rare; deformation twins on {0001}            |  
 |  |   Extinction  | Symmetrical to cleavage traces in sections subparallel to c. Mottled extinction due to preparation-related, miniscule surface breakouts at cleavage intersections            |  
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|   Reaction textures   |             |  
 |  |   Alteration /   decomposition  | Soluble            |  
 |  
 
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|   Occurence    |   Ign  |             |  
 |  |  |   Met  | Aggregates and disseminated grains in serpentinite and other Mg-rich rocks; metasomatic zones between calcareous rocks and intrusions            |  
 |  |  |   Sed  | Evaporitic deposits; interaction of Mg-rich brines with carbonate sediments; magnesite deposits from near-surface alteration of Mg-rich ultramafic rocks, such as serpentinites, peridotites, pyroxenites, dunites         |  
 |  |  |   Hyd  | Veins in Mg-rich rocks, amygdales in mafic volcanics            |  
 |  |  |   Other  |             |  
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|   Distinctive   properties                | High-order white interference colours, rhombohedral cleavage and relief change between nO and nE (as for all other rhombohedral carbonates). Lacks the lamellar twins that are characteristic for calcite and dolomite; occurrence restricted to Mg-rich rocks.          |  
 |  |   Additional   comments  | n-Δn chart: Cal - calcite, Dol - dolomite, Kut - kutnahorite, Mgs - magnesite, Rds - rhodochrosite, Sid - siderite, Smt - smithsonite                     |  
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