Standard

Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform. / Savelev, A. D.; Yu Lebedeva, O.

в: IOP Conference Series: Earth and Environmental Science , Том 319, № 1, 012017, 19.09.2019.

Результаты исследований: Научные публикации в периодических изданияхстатья в журнале по материалам конференцииРецензирование

Harvard

Savelev, AD & Yu Lebedeva, O 2019, 'Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform', IOP Conference Series: Earth and Environmental Science , Том. 319, № 1, 012017. https://doi.org/10.1088/1755-1315/319/1/012017

APA

Vancouver

Savelev AD, Yu Lebedeva O. Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform. IOP Conference Series: Earth and Environmental Science . 2019 Сент. 19;319(1). 012017. https://doi.org/10.1088/1755-1315/319/1/012017

Author

Savelev, A. D. ; Yu Lebedeva, O. / Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform. в: IOP Conference Series: Earth and Environmental Science . 2019 ; Том 319, № 1.

BibTeX

@article{cf3f741e179f4b6299bf100dd8beff29,
title = "Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform",
abstract = "Geochemical study of mafic dikes and sills of the Riphean (Ulakhanbam) and Ordovician (Suordakh) ages in the area of the Sette-Daban ridge allowed to establish differences between these complexes. For the Ulakhanbam magmatic rocks, the mantle source was basically similar in characteristics to E-MORB. Despite the possible sediment contamination, wide range of ϵNd(T) values is most likely due to the specific composition of the mantle source, which likely had an admixture of OIB material. The Ordovician reservoir had OIB characteristics, whereas the MORB material had a subordinate significance.",
author = "Savelev, {A. D.} and {Yu Lebedeva}, O.",
note = "Publisher Copyright: {\textcopyright} 2019 IOP Publishing Ltd. All rights reserved.; 10th All Russian Petrographic Conference with International Participationon Petrology of Magnetic and Metamorphic Complexes ; Conference date: 27-11-2018 Through 28-11-2018",
year = "2019",
month = sep,
day = "19",
doi = "10.1088/1755-1315/319/1/012017",
language = "English",
volume = "319",
journal = "IOP Conference Series: Earth and Environmental Science",
issn = "1755-1307",
publisher = "IOP Publishing Ltd.",
number = "1",

}

RIS

TY - JOUR

T1 - Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform

AU - Savelev, A. D.

AU - Yu Lebedeva, O.

N1 - Publisher Copyright: © 2019 IOP Publishing Ltd. All rights reserved.

PY - 2019/9/19

Y1 - 2019/9/19

N2 - Geochemical study of mafic dikes and sills of the Riphean (Ulakhanbam) and Ordovician (Suordakh) ages in the area of the Sette-Daban ridge allowed to establish differences between these complexes. For the Ulakhanbam magmatic rocks, the mantle source was basically similar in characteristics to E-MORB. Despite the possible sediment contamination, wide range of ϵNd(T) values is most likely due to the specific composition of the mantle source, which likely had an admixture of OIB material. The Ordovician reservoir had OIB characteristics, whereas the MORB material had a subordinate significance.

AB - Geochemical study of mafic dikes and sills of the Riphean (Ulakhanbam) and Ordovician (Suordakh) ages in the area of the Sette-Daban ridge allowed to establish differences between these complexes. For the Ulakhanbam magmatic rocks, the mantle source was basically similar in characteristics to E-MORB. Despite the possible sediment contamination, wide range of ϵNd(T) values is most likely due to the specific composition of the mantle source, which likely had an admixture of OIB material. The Ordovician reservoir had OIB characteristics, whereas the MORB material had a subordinate significance.

UR - http://www.scopus.com/inward/record.url?scp=85073079559&partnerID=8YFLogxK

U2 - 10.1088/1755-1315/319/1/012017

DO - 10.1088/1755-1315/319/1/012017

M3 - Conference article

AN - SCOPUS:85073079559

VL - 319

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

SN - 1755-1307

IS - 1

M1 - 012017

T2 - 10th All Russian Petrographic Conference with International Participationon Petrology of Magnetic and Metamorphic Complexes

Y2 - 27 November 2018 through 28 November 2018

ER -

ID: 92279013