| 1. | Within the Zazhoginskoe field are carbonate, sericite, albite and quartz.
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| 2. | Fresh mineral alteration has occurred as sericite, serpentine, and chlorite are found.
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| 3. | Millimetre-sized shear bands within the G�nis sericite schist also point at dextral shearing.
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| 4. | Minerals produced by alteration include calcite, chlorite, epidote, kaolinite, rutile and sericite.
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| 5. | The selvages are generally < 10 cm in diameter and composed of major sericite and minor quartz.
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| 6. | Beginning in 1951, the deposit was mined for associated sericite, which was used as a white filler.
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| 7. | These rocks are regarded as metamorphosed sediments containing a laminate of graphite, mica quartz-sericite and sericite schists.
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| 8. | These rocks are regarded as metamorphosed sediments containing a laminate of graphite, mica quartz-sericite and sericite schists.
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| 9. | Alteration is nonexistent to very weak at best and the weak chlorite and sericite are believed to be mainly post-ore effects.
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| 10. | Plagioclase will be altered to sericite ( a fine-grained white mica ) by sericitic alteration, and mafic minerals are replaced by quartz.
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