High-temperature aquamarine from vugless granite pegmatites of the Suprunovskoye deposit Irkutsk oblast, Russia
Keyword(s):
New data on the chemical composition were obtained for the aquamarine of the Suprunovskoye deposit: SiO2 66.10; Na2O 0.51; Al2O3 17.99; MgO 0.37; K2O 0.03; CaO 0.02; FeO 0.58; BeOcalc. 13.70 (wt%) and fluid and melt inclusions were investigated. Defined that aquamarine was formed in the late stages of granitic magmatism from a specific pegmatite silicate melt or water-silicate liquid enriched with water (>7 wt%), heavy REE (La/Yb = 0.48), lithium, but depleted in fluorine and boron at temperatures of about 700ºС and a pressure of about 6 kbar.
1997 ◽
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pp. 2569-2575
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2011 ◽
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pp. 1368-1377
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1962 ◽
Vol 84
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pp. 223-257
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1996 ◽
Vol 60
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pp. 2257-2263
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2018 ◽
Vol 383
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pp. 31-35
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