We have achieved expertise in the manufacturing of Garnets etc. We have firmly positioned ourselves as the most preeminent octagon garnet manufacturer and one of the dominant garnet stones manufacturers and exporters from India. Color Specification :

• Grossular garnets of yellow-orange to orange-red to brown colors are known as hessonite garnets.
• Garnet is allochromatic, meaning that most of the color variations in different garnets are due to their highly variable trace element impurities rather than to their bulk composition elements.
• The color we see in garnets is produced when light is selectively absorbed by these ions or by interactions between these ions (intervalent charge transfers).

• Garnets form in a variety of geologic settings, depending on the garnet species.
• It occurs in schists and gneisses, resulting from regional metamorphism of argillaceous sediments.
• It is a characteristic mineral constituent of the amphibolite metamorphic phases, also appearing in the granulate faces. Almandine also occurs in pegmatite dikes and in some granitic and volcanic rocks, as well as in sedimentary deposits as detrital grains.
• It is characteristic of ultra-mafic rocks such as peridotites, kimberlitic, eclogites and serpentines, and in sedimentary deposits derived from their weathering.
• Occurs in granitic pegmaties and in skarns, also found in sedimentary deposits.

We have achieved expertise in the manufacturing of Garnets etc. We have firmly positioned ourselves as the most preeminent octagon garnet manufacturer and one of the dominant garnet stones manufacturers and exporters from India. Color Specification :

• Grossular garnets of yellow-orange to orange-red to brown colors are known as hessonite garnets.
• Garnet is allochromatic, meaning that most of the color variations in different garnets are due to their highly variable trace element impurities rather than to their bulk composition elements.
• The color we see in garnets is produced when light is selectively absorbed by these ions or by interactions between these ions (intervalent charge transfers).

• Garnets form in a variety of geologic settings, depending on the garnet species.
• It occurs in schists and gneisses, resulting from regional metamorphism of argillaceous sediments.
• It is a characteristic mineral constituent of the amphibolite metamorphic phases, also appearing in the granulate faces. Almandine also occurs in pegmatite dikes and in some granitic and volcanic rocks, as well as in sedimentary deposits as detrital grains.
• It is characteristic of ultra-mafic rocks such as peridotites, kimberlitic, eclogites and serpentines, and in sedimentary deposits derived from their weathering.
• Occurs in granitic pegmaties and in skarns, also found in sedimentary deposits.