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Paleozoic dike series in the Kola Alkaline Province : Age and characteristics of mantle sources. / Arzamastsev, A. A.; Travin, A. V.; Belyatskii, B. V.; Arzamastseva, L. V.

в: Doklady Earth Sciences, Том 391, № 6, 01.07.2003, стр. 906-909.

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

Harvard

Arzamastsev, AA, Travin, AV, Belyatskii, BV & Arzamastseva, LV 2003, 'Paleozoic dike series in the Kola Alkaline Province: Age and characteristics of mantle sources', Doklady Earth Sciences, Том. 391, № 6, стр. 906-909.

APA

Arzamastsev, A. A., Travin, A. V., Belyatskii, B. V., & Arzamastseva, L. V. (2003). Paleozoic dike series in the Kola Alkaline Province: Age and characteristics of mantle sources. Doklady Earth Sciences, 391(6), 906-909.

Vancouver

Arzamastsev AA, Travin AV, Belyatskii BV, Arzamastseva LV. Paleozoic dike series in the Kola Alkaline Province: Age and characteristics of mantle sources. Doklady Earth Sciences. 2003 Июль 1;391(6):906-909.

Author

Arzamastsev, A. A. ; Travin, A. V. ; Belyatskii, B. V. ; Arzamastseva, L. V. / Paleozoic dike series in the Kola Alkaline Province : Age and characteristics of mantle sources. в: Doklady Earth Sciences. 2003 ; Том 391, № 6. стр. 906-909.

BibTeX

@article{7d305a21851047b7a231734218f375bd,
title = "Paleozoic dike series in the Kola Alkaline Province: Age and characteristics of mantle sources",
abstract = "In order to date the cessation of magmatic activity and characterize the final stage of Paleozoic magmatism in the northeast Baltic Shield, we carried out isotope-geochemical investigation of dikes that are abundant within the Kola region. Alkaline dikes are complex objects for dating. They lack zircon but contain alien mantle material and lower crustal xenoliths. Moreover, they are characternized by postmagmatic alterations and wall-rock assimilation. Therefore, we used a combination of Rb-Sr and Sm-Nd isochron determinations (internal mineral isochron) and 40Ar/39Ar methods These methods are described.",
author = "Arzamastsev, {A. A.} and Travin, {A. V.} and Belyatskii, {B. V.} and Arzamastseva, {L. V.}",
year = "2003",
month = jul,
day = "1",
language = "English",
volume = "391",
pages = "906--909",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Paleozoic dike series in the Kola Alkaline Province

T2 - Age and characteristics of mantle sources

AU - Arzamastsev, A. A.

AU - Travin, A. V.

AU - Belyatskii, B. V.

AU - Arzamastseva, L. V.

PY - 2003/7/1

Y1 - 2003/7/1

N2 - In order to date the cessation of magmatic activity and characterize the final stage of Paleozoic magmatism in the northeast Baltic Shield, we carried out isotope-geochemical investigation of dikes that are abundant within the Kola region. Alkaline dikes are complex objects for dating. They lack zircon but contain alien mantle material and lower crustal xenoliths. Moreover, they are characternized by postmagmatic alterations and wall-rock assimilation. Therefore, we used a combination of Rb-Sr and Sm-Nd isochron determinations (internal mineral isochron) and 40Ar/39Ar methods These methods are described.

AB - In order to date the cessation of magmatic activity and characterize the final stage of Paleozoic magmatism in the northeast Baltic Shield, we carried out isotope-geochemical investigation of dikes that are abundant within the Kola region. Alkaline dikes are complex objects for dating. They lack zircon but contain alien mantle material and lower crustal xenoliths. Moreover, they are characternized by postmagmatic alterations and wall-rock assimilation. Therefore, we used a combination of Rb-Sr and Sm-Nd isochron determinations (internal mineral isochron) and 40Ar/39Ar methods These methods are described.

UR - http://www.scopus.com/inward/record.url?scp=0141682748&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0141563196

VL - 391

SP - 906

EP - 909

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 6

ER -

ID: 34786280