Standard

Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis). / Vasil’ev, Yu R.; Gora, M. P.; Kuzmin, D. V.

в: Doklady Earth Sciences, Том 478, № 1, 01.01.2018, стр. 103-107.

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

Harvard

Vasil’ev, YR, Gora, MP & Kuzmin, DV 2018, 'Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis)', Doklady Earth Sciences, Том. 478, № 1, стр. 103-107. https://doi.org/10.1134/S1028334X18010282

APA

Vasil’ev, Y. R., Gora, M. P., & Kuzmin, D. V. (2018). Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis). Doklady Earth Sciences, 478(1), 103-107. https://doi.org/10.1134/S1028334X18010282

Vancouver

Vasil’ev YR, Gora MP, Kuzmin DV. Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis). Doklady Earth Sciences. 2018 янв. 1;478(1):103-107. doi: 10.1134/S1028334X18010282

Author

Vasil’ev, Yu R. ; Gora, M. P. ; Kuzmin, D. V. / Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis). в: Doklady Earth Sciences. 2018 ; Том 478, № 1. стр. 103-107.

BibTeX

@article{fff5fef0022c49f898c31d31a80e8a7c,
title = "Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis)",
abstract = "For the Permian–Triassic foidite and meimechite lavas of Polar Siberia, both the whole-rock petrochemistry and geochemistry and that of melt inclusions in olivine phenocrysts from the same rocks have been demonstrated to be similar. In addition, their isotope characteristics imply the possibility of their generation from an abyssal parental melt compositionally resembling a high–Mg alkaline picrite.",
author = "Vasil{\textquoteright}ev, {Yu R.} and Gora, {M. P.} and Kuzmin, {D. V.}",
year = "2018",
month = jan,
day = "1",
doi = "10.1134/S1028334X18010282",
language = "English",
volume = "478",
pages = "103--107",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis)

AU - Vasil’ev, Yu R.

AU - Gora, M. P.

AU - Kuzmin, D. V.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - For the Permian–Triassic foidite and meimechite lavas of Polar Siberia, both the whole-rock petrochemistry and geochemistry and that of melt inclusions in olivine phenocrysts from the same rocks have been demonstrated to be similar. In addition, their isotope characteristics imply the possibility of their generation from an abyssal parental melt compositionally resembling a high–Mg alkaline picrite.

AB - For the Permian–Triassic foidite and meimechite lavas of Polar Siberia, both the whole-rock petrochemistry and geochemistry and that of melt inclusions in olivine phenocrysts from the same rocks have been demonstrated to be similar. In addition, their isotope characteristics imply the possibility of their generation from an abyssal parental melt compositionally resembling a high–Mg alkaline picrite.

UR - http://www.scopus.com/inward/record.url?scp=85042556256&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18010282

DO - 10.1134/S1028334X18010282

M3 - Article

AN - SCOPUS:85042556256

VL - 478

SP - 103

EP - 107

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 12101327