Standard

High-Temperature Beryl from Vugless Granite Pegmatites of the Suprunovskoye Deposit, Irkutsk Oblast, Russia. / Gerasimova, E. I.; Prokof’iev, V. Yu; Smirnov, S. Z. et al.

In: Geochemistry International, Vol. 57, No. 7, 01.07.2019, p. 829-834.

Research output: Contribution to journal › Article › peer-review

Harvard

Gerasimova, EI, Prokof’iev, VY, Smirnov, SZ & Kovalskaya, TN 2019, 'High-Temperature Beryl from Vugless Granite Pegmatites of the Suprunovskoye Deposit, Irkutsk Oblast, Russia', Geochemistry International, vol. 57, no. 7, pp. 829-834. https://doi.org/10.1134/S001670291907005X

APA

Gerasimova, E. I., Prokof’iev, V. Y., Smirnov, S. Z., & Kovalskaya, T. N. (2019). High-Temperature Beryl from Vugless Granite Pegmatites of the Suprunovskoye Deposit, Irkutsk Oblast, Russia. Geochemistry International, 57(7), 829-834. https://doi.org/10.1134/S001670291907005X

Vancouver

Gerasimova EI, Prokof’iev VY, Smirnov SZ, Kovalskaya TN. High-Temperature Beryl from Vugless Granite Pegmatites of the Suprunovskoye Deposit, Irkutsk Oblast, Russia. Geochemistry International. 2019 Jul 1;57(7):829-834. doi: 10.1134/S001670291907005X

Author

Gerasimova, E. I. ; Prokof’iev, V. Yu ; Smirnov, S. Z. et al. / High-Temperature Beryl from Vugless Granite Pegmatites of the Suprunovskoye Deposit, Irkutsk Oblast, Russia. In: Geochemistry International. 2019 ; Vol. 57, No. 7. pp. 829-834.

BibTeX

@article{77e48975d91d4c6086401af19e8881c3,
title = "High-Temperature Beryl from Vugless Granite Pegmatites of the Suprunovskoye Deposit, Irkutsk Oblast, Russia",
abstract = "New data were obtained on the chemical composition of beryl from the Suprunovskoye deposit (wt %): 66.10 SiO2, 0.51 Na2O, 17.99 Al2O3, 0.37 MgO, 0.03 K2O, 0.02 CaO, 0.58 FeO, and 13.70 BeO (calculated). Fluid and melt inclusions were investigated for the first time in this mineral. It was found that the beryl was formed during late stages of granite magmatism from a specific pegmatite silicate melt or a water–silicate liquid enriched in water (>7 wt %), heavy REE (La/Yb = 0.48), and lithium, and depleted in fluorine and boron at a temperature of ~700°C and a pressure of ~6 kbar.",
keywords = "aquamarine, beryl, granite magmatism, Irel complex, melt inclusion, Suprunovskoye deposit, vugless pegmatite, HYDROSILICATE LIQUIDS, MAGMAS, WATER",
author = "Gerasimova, {E. I.} and Prokof{\textquoteright}iev, {V. Yu} and Smirnov, {S. Z.} and Kovalskaya, {T. N.}",
note = "Publisher Copyright: {\textcopyright} 2019, Pleiades Publishing, Ltd.",
year = "2019",
month = jul,
day = "1",
doi = "10.1134/S001670291907005X",
language = "English",
volume = "57",
pages = "829--834",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "PLEIADES PUBLISHING INC",
number = "7",

}

RIS

TY - JOUR

T1 - High-Temperature Beryl from Vugless Granite Pegmatites of the Suprunovskoye Deposit, Irkutsk Oblast, Russia

AU - Gerasimova, E. I.

AU - Prokof’iev, V. Yu

AU - Smirnov, S. Z.

AU - Kovalskaya, T. N.

N1 - Publisher Copyright: © 2019, Pleiades Publishing, Ltd.

PY - 2019/7/1

Y1 - 2019/7/1

N2 - New data were obtained on the chemical composition of beryl from the Suprunovskoye deposit (wt %): 66.10 SiO2, 0.51 Na2O, 17.99 Al2O3, 0.37 MgO, 0.03 K2O, 0.02 CaO, 0.58 FeO, and 13.70 BeO (calculated). Fluid and melt inclusions were investigated for the first time in this mineral. It was found that the beryl was formed during late stages of granite magmatism from a specific pegmatite silicate melt or a water–silicate liquid enriched in water (>7 wt %), heavy REE (La/Yb = 0.48), and lithium, and depleted in fluorine and boron at a temperature of ~700°C and a pressure of ~6 kbar.

AB - New data were obtained on the chemical composition of beryl from the Suprunovskoye deposit (wt %): 66.10 SiO2, 0.51 Na2O, 17.99 Al2O3, 0.37 MgO, 0.03 K2O, 0.02 CaO, 0.58 FeO, and 13.70 BeO (calculated). Fluid and melt inclusions were investigated for the first time in this mineral. It was found that the beryl was formed during late stages of granite magmatism from a specific pegmatite silicate melt or a water–silicate liquid enriched in water (>7 wt %), heavy REE (La/Yb = 0.48), and lithium, and depleted in fluorine and boron at a temperature of ~700°C and a pressure of ~6 kbar.

KW - aquamarine

KW - beryl

KW - granite magmatism

KW - Irel complex

KW - melt inclusion

KW - Suprunovskoye deposit

KW - vugless pegmatite

KW - HYDROSILICATE LIQUIDS

KW - MAGMAS

KW - WATER

UR - http://www.scopus.com/inward/record.url?scp=85068563349&partnerID=8YFLogxK

U2 - 10.1134/S001670291907005X

DO - 10.1134/S001670291907005X

M3 - Article

AN - SCOPUS:85068563349

VL - 57

SP - 829

EP - 834

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 7

ER -

ID: 25761989