Standard

Zircons from a pegmatite cutting eclogite (Gridino, belomorian mobile belt): U-pb-o and trace element constraints on eclogite metamorphism and fluid activity. / Skublov, S.G.; Berezin, A.V.; SALIMGARAEVA , L.I.; LI , X.H.; LI , Q.L.; TRAVIN , V.V.; REZVUKHIN , D.I.

в: Geosciences (Switzerland), Том 10, № 5, 21.05.2020, стр. 197.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Skublov, SG, Berezin, AV, SALIMGARAEVA , LI, LI , XH, LI , QL, TRAVIN , VV & REZVUKHIN , DI 2020, 'Zircons from a pegmatite cutting eclogite (Gridino, belomorian mobile belt): U-pb-o and trace element constraints on eclogite metamorphism and fluid activity.', Geosciences (Switzerland), Том. 10, № 5, стр. 197. https://doi.org/10.3390/geosciences10050197

APA

Skublov, S. G., Berezin, A. V., SALIMGARAEVA , L. I., LI , X. H., LI , Q. L., TRAVIN , V. V., & REZVUKHIN , D. I. (2020). Zircons from a pegmatite cutting eclogite (Gridino, belomorian mobile belt): U-pb-o and trace element constraints on eclogite metamorphism and fluid activity. Geosciences (Switzerland), 10(5), 197. https://doi.org/10.3390/geosciences10050197

Vancouver

Skublov SG, Berezin AV, SALIMGARAEVA LI, LI XH, LI QL, TRAVIN VV и пр. Zircons from a pegmatite cutting eclogite (Gridino, belomorian mobile belt): U-pb-o and trace element constraints on eclogite metamorphism and fluid activity. Geosciences (Switzerland). 2020 Май 21;10(5):197. https://doi.org/10.3390/geosciences10050197

Author

Skublov, S.G. ; Berezin, A.V. ; SALIMGARAEVA , L.I. ; LI , X.H. ; LI , Q.L. ; TRAVIN , V.V. ; REZVUKHIN , D.I. / Zircons from a pegmatite cutting eclogite (Gridino, belomorian mobile belt): U-pb-o and trace element constraints on eclogite metamorphism and fluid activity. в: Geosciences (Switzerland). 2020 ; Том 10, № 5. стр. 197.

BibTeX

@article{f855b0420c834c5a910070c212ef0cf5,
title = "Zircons from a pegmatite cutting eclogite (Gridino, belomorian mobile belt): U-pb-o and trace element constraints on eclogite metamorphism and fluid activity.",
abstract = "This report presents new data on U-Pb geochronology, oxygen isotopes, and trace element composition of zircon from a pegmatite vein crosscutting an eclogite boudin on Stolbikha Island, Gridino area, Belomorian mobile belt (BMB). The zircon grains occur as two distinct populations. The predominant population is pegmatitic and shows dark cathodoluminescence (CL); about a third of this population contains inherited cores. The second zircon population is typical of granulite and exhibits a well-defined sectorial (mosaic) zoning in CL. Both the inherited cores and sectorial in CL zircons appear to have been captured from metabasites as xenocrysts during the pegmatite vein formation. A U-Pb age of 1890 ± 2 Ma for the main zircon population is interpreted as the age of the pegmatite injection. This value is close to the age threshold for the BMB eclogites (~1.9 Ga) and unambiguously defines the upper age limit for the eclogite metamorphism. The pegmatite formation is thus related to partial melting events that occur",
author = "S.G. Skublov and A.V. Berezin and L.I. SALIMGARAEVA and X.H. LI and Q.L. LI and V.V. TRAVIN and D.I. REZVUKHIN",
year = "2020",
month = may,
day = "21",
doi = "10.3390/geosciences10050197",
language = "English",
volume = "10",
pages = "197",
journal = "Geosciences (Switzerland)",
issn = "2076-3263",
publisher = "MDPI AG",
number = "5",

}

RIS

TY - JOUR

T1 - Zircons from a pegmatite cutting eclogite (Gridino, belomorian mobile belt): U-pb-o and trace element constraints on eclogite metamorphism and fluid activity.

AU - Skublov, S.G.

AU - Berezin, A.V.

AU - SALIMGARAEVA , L.I.

AU - LI , X.H.

AU - LI , Q.L.

AU - TRAVIN , V.V.

AU - REZVUKHIN , D.I.

PY - 2020/5/21

Y1 - 2020/5/21

N2 - This report presents new data on U-Pb geochronology, oxygen isotopes, and trace element composition of zircon from a pegmatite vein crosscutting an eclogite boudin on Stolbikha Island, Gridino area, Belomorian mobile belt (BMB). The zircon grains occur as two distinct populations. The predominant population is pegmatitic and shows dark cathodoluminescence (CL); about a third of this population contains inherited cores. The second zircon population is typical of granulite and exhibits a well-defined sectorial (mosaic) zoning in CL. Both the inherited cores and sectorial in CL zircons appear to have been captured from metabasites as xenocrysts during the pegmatite vein formation. A U-Pb age of 1890 ± 2 Ma for the main zircon population is interpreted as the age of the pegmatite injection. This value is close to the age threshold for the BMB eclogites (~1.9 Ga) and unambiguously defines the upper age limit for the eclogite metamorphism. The pegmatite formation is thus related to partial melting events that occur

AB - This report presents new data on U-Pb geochronology, oxygen isotopes, and trace element composition of zircon from a pegmatite vein crosscutting an eclogite boudin on Stolbikha Island, Gridino area, Belomorian mobile belt (BMB). The zircon grains occur as two distinct populations. The predominant population is pegmatitic and shows dark cathodoluminescence (CL); about a third of this population contains inherited cores. The second zircon population is typical of granulite and exhibits a well-defined sectorial (mosaic) zoning in CL. Both the inherited cores and sectorial in CL zircons appear to have been captured from metabasites as xenocrysts during the pegmatite vein formation. A U-Pb age of 1890 ± 2 Ma for the main zircon population is interpreted as the age of the pegmatite injection. This value is close to the age threshold for the BMB eclogites (~1.9 Ga) and unambiguously defines the upper age limit for the eclogite metamorphism. The pegmatite formation is thus related to partial melting events that occur

U2 - 10.3390/geosciences10050197

DO - 10.3390/geosciences10050197

M3 - Article

VL - 10

SP - 197

JO - Geosciences (Switzerland)

JF - Geosciences (Switzerland)

SN - 2076-3263

IS - 5

ER -

ID: 78512067