SOME MINERAL-GEOCHEMISTRY ASPECTS OF BERYLL BELOKURICHINSKII PLUTON OF GORNY ALTAY DOI Open Access

А. И. Гусев,

O.S. Kolyvanova

International Journal of Applied and Fundamental Research (Международный журнал прикладных и фундаментальных исследований), Journal Year: 2024, Volume and Issue: №4 2024, P. 16 - 20

Published: Jan. 1, 2024

НЕКОТОРЫЕ МИНЕРАЛОГО-ГЕОХИМИЧЕСКИЕ АСПЕКТЫ БЕРИЛЛА БЕЛОКУРИХИНСКОГО ПЛУТОНА ГОРНОГО АЛТАЯГусев А

Language: Русский

Formation of the Mahuaping Be–W–F deposit in South China: Evidence from beryl chemistry, wolframite and monazite U–Pb dating DOI Creative Commons

Wenchang Li,

Qinggao Yan,

Huawen Cao

et al.

Ore Geology Reviews, Journal Year: 2025, Volume and Issue: unknown, P. 106553 - 106553

Published: March 1, 2025

Language: Английский

Citations

0
Contribution of pegmatite shells to magmatic evolution and rare metal mineralization: Insights from the Shihuiyao deposit, Inner Mongolia, Northeast China DOI Creative Commons
Zhichao Zhang, Zheng Ji,

Yusheng Zhu

et al.

Geoscience Frontiers, Journal Year: 2025, Volume and Issue: unknown, P. 102042 - 102042

Published: March 1, 2025

Language: Английский

Citations

0
Micro‐Raman Spectroscopy Characterization of Emeralds Combined With LA‐ICP‐MS Analysis and Multivariate Statistical Methods DOI
Raquel Alonso‐Perez,

Adriana Heimann Ríos,

Daniel X. Gray

et al.

Journal of Raman Spectroscopy, Journal Year: 2025, Volume and Issue: unknown

Published: April 10, 2025

ABSTRACT Gem‐quality emeralds—the green color variety of beryl (Be 3 Al 2 Si 6 O 18 )—from some the most important world localities (Australia, Austria, Brazil, China, Colombia, Egypt, Madagascar, Nigeria, Russia, South Africa, and Zambia) were characterized using micro‐Raman spectroscopy. There are three main characteristic Raman shift regions in emeralds: fingerprint region (150–1500 cm −1 ) representative Si‐O, Be‐O, Al‐O bonds; water (3500–3900 ), nitrogen hydrocarbons (~2325 ~2914 , respectively). This study examined crystals gemstones representing 11 major along with one synthetic. The analysis involved a systematic crystal orientation effects (parallel perpendicular to c ‐axis) peak finding fitting center full width half maximum peaks Fourier self‐deconvolution Lorentz functions, respectively. Peak intensity was found be strongly influenced by polarization effects, bands around 1070 due Si‐O and/or Be‐O stretching, being affected. Colombian emeralds, carbonaceous black shales low alkalis, exhibited dominant type‐I (3608 both orientations showed highest N molecule ). In contrast, Madagascar Zambian emeralds had type‐II (3598 alkali concentrations. Preliminary linear discriminant (LDA) applied spectroscopy LA‐ICPMS datasets demonstrates distinct clustering pattern for emeralds. Furthermore, effectively differentiates Pan‐African deposits, specifically distinguishing Madagascan samples from ones. Including additional combined other would enhance potential as provenance tool.

Language: Английский

Citations

0
Trace element zoning of colorless beryl from spodumene pegmatites of Pashki deposit (Nuristan province, Afghanistan) DOI Creative Commons
С. Г. Скублов,

Nazifullah Hamdard,

Mikhail Ivanov

et al.

Frontiers in Earth Science, Journal Year: 2024, Volume and Issue: 12

Published: July 25, 2024

Trace element zoning of colorless beryl from spodumene pegmatites Pashki deposit (Nuristan province, Afghanistan)

Language: Английский

Citations

3
Crystallographic insights and crystal fractionation simulations of alkali- and water-bearing beryl: Implications for magmatic–hydrothermal evolution and Be enrichment mechanisms DOI Creative Commons

Zhiwei Fan,

Yi-Qu Xiong, Matthew J. Brzozowski

et al.

Ore Geology Reviews, Journal Year: 2024, Volume and Issue: unknown, P. 106278 - 106278

Published: Oct. 1, 2024

Language: Английский

Citations

2
Trace element composition of beryl from spodumene pegmatite deposits of the Kunar Province, Afghanistan DOI
С. Г. Скублов, Ataullah Yosufzai, А. А. Евдокимов

et al.

МИНЕРАЛОГИЯ (MINERALOGY), Journal Year: 2024, Volume and Issue: 10(2), P. 58 - 77

Published: July 3, 2024

The study of trace element composition beryl from the Chambalak and Digal deposits Darai Pech pegmatite feld Kunar province (Afghanistan) using secondary ion mass spectrometry (SIMS) revealed sectoriality crystal deposit. inner outer parts profle are identifed as pinacoid (0001) prism (10 1 0) growth zones, respectively. At boundary these two simple forms, Cs, Na, Ca, Fe, Mg, V content strongly increases. zone exhibits pyramids: a decrease in V, Ni, Cr during towards edge crystal. H2O Mg increases zone. No between zones is observed There reason to consider its A comparison based on indicative elements, increase which corresponds fractionation trend melt (Cs, Li, Rb), with other objects showed that studied was moderately fractionated corresponding initial evolution stages. It shown some elements can fundamentally differ.

Language: Английский

Citations

1
SOME MINERAL-GEOCHEMISTRY ASPECTS OF BERYLL BELOKURICHINSKII PLUTON OF GORNY ALTAY DOI Open Access

А. И. Гусев,

O.S. Kolyvanova

International Journal of Applied and Fundamental Research (Международный журнал прикладных и фундаментальных исследований), Journal Year: 2024, Volume and Issue: №4 2024, P. 16 - 20

Published: Jan. 1, 2024

НЕКОТОРЫЕ МИНЕРАЛОГО-ГЕОХИМИЧЕСКИЕ АСПЕКТЫ БЕРИЛЛА БЕЛОКУРИХИНСКОГО ПЛУТОНА ГОРНОГО АЛТАЯГусев А

Language: Русский

Citations

0