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Member Since 18 Years
Nature of Business Exporter Year of Establishment 1980Ask for more detail from the seller
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Graphite most commonly occurs in metamorphic rocks, such as crystalline limestones, schists and gneisses. It may occur as large crystalline plates. It has probably been derived from carbon material of organic origin which has been converted into graphite during the metamorphism of the rock. Coal beds, under influence or strong metamorphic action, such as the intrusion into them of an igneous rock, have in a greater or less degree been converted into graphitic.
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Ingredients | Upto- 84% | 85 – 88% | 88 – 89% | 90% | 91% | 92% | 93% | 94% | 95% | 96% | |
Volatile Matter (V.M.) (Max.) | 4.5 | 4.0 | 3.5 | 3.0 | 3.0 | 2.5 | 2.5 | 2.0 | 2.0 | 2.0 | |
Ash Content | 12.0 | 10.5 | 8.5 | 7.5 | 6.5 | 6.5 | 5.5 | 4.5 | 3.5 | 3.0 | |
V.M. + ASH (Max.) | 15.5 | 14.5 | 11.5 | 9.5 | 8.5 | 7.5 | 6.5 | 5.5 | 4.5 | 3.5 | |
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