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First findings of the volcanic rocks in Svecofennides of the Ladoga region and their age. / Baltybaev, Sh K.; Levchenko, O. A.; Galankina, O. L.

в: Doklady Earth Sciences, Том 395, № 3, 2004, стр. 311-314.

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

Harvard

Baltybaev, SK, Levchenko, OA & Galankina, OL 2004, 'First findings of the volcanic rocks in Svecofennides of the Ladoga region and their age', Doklady Earth Sciences, Том. 395, № 3, стр. 311-314.

APA

Baltybaev, S. K., Levchenko, O. A., & Galankina, O. L. (2004). First findings of the volcanic rocks in Svecofennides of the Ladoga region and their age. Doklady Earth Sciences, 395(3), 311-314.

Vancouver

Baltybaev SK, Levchenko OA, Galankina OL. First findings of the volcanic rocks in Svecofennides of the Ladoga region and their age. Doklady Earth Sciences. 2004;395(3):311-314.

Author

Baltybaev, Sh K. ; Levchenko, O. A. ; Galankina, O. L. / First findings of the volcanic rocks in Svecofennides of the Ladoga region and their age. в: Doklady Earth Sciences. 2004 ; Том 395, № 3. стр. 311-314.

BibTeX

@article{3cbe8b03878b4be5b6410fa7ee6a6af9,
title = "First findings of the volcanic rocks in Svecofennides of the Ladoga region and their age",
abstract = "Svecofennides occupy a vast territory in the southeastern Baltic Shield. They are distributed mainly in the Scandinavian and Baltic countries. In Russia, they are developed only within the Ladoga region. Scandinavian geologists have shown that tectonic relations between Svecofennian rocks and the adjacent Archean infracrustal complex can be characterized in terms of the ocean-continent boundary. Based on U-Pb zircon dating of the underlying amphibolites of the Sortavala Group, the age of metaturbidites of the Ladoga region is estimated to be no older than 1.96 Ga [8]. The upper age was constrained by the crystallization age of norite-enderbite rocks crosscutting the metaturbidite sequence (1.88-1.89 Ga). The U-Pb dating of zircons and monazites from metamorphic rocks and migmatites suggests a metamorphic peak of the turbidite sequences at 1.87-1.88 Ga.",
author = "Baltybaev, {Sh K.} and Levchenko, {O. A.} and Galankina, {O. L.}",
year = "2004",
language = "English",
volume = "395",
pages = "311--314",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - First findings of the volcanic rocks in Svecofennides of the Ladoga region and their age

AU - Baltybaev, Sh K.

AU - Levchenko, O. A.

AU - Galankina, O. L.

PY - 2004

Y1 - 2004

N2 - Svecofennides occupy a vast territory in the southeastern Baltic Shield. They are distributed mainly in the Scandinavian and Baltic countries. In Russia, they are developed only within the Ladoga region. Scandinavian geologists have shown that tectonic relations between Svecofennian rocks and the adjacent Archean infracrustal complex can be characterized in terms of the ocean-continent boundary. Based on U-Pb zircon dating of the underlying amphibolites of the Sortavala Group, the age of metaturbidites of the Ladoga region is estimated to be no older than 1.96 Ga [8]. The upper age was constrained by the crystallization age of norite-enderbite rocks crosscutting the metaturbidite sequence (1.88-1.89 Ga). The U-Pb dating of zircons and monazites from metamorphic rocks and migmatites suggests a metamorphic peak of the turbidite sequences at 1.87-1.88 Ga.

AB - Svecofennides occupy a vast territory in the southeastern Baltic Shield. They are distributed mainly in the Scandinavian and Baltic countries. In Russia, they are developed only within the Ladoga region. Scandinavian geologists have shown that tectonic relations between Svecofennian rocks and the adjacent Archean infracrustal complex can be characterized in terms of the ocean-continent boundary. Based on U-Pb zircon dating of the underlying amphibolites of the Sortavala Group, the age of metaturbidites of the Ladoga region is estimated to be no older than 1.96 Ga [8]. The upper age was constrained by the crystallization age of norite-enderbite rocks crosscutting the metaturbidite sequence (1.88-1.89 Ga). The U-Pb dating of zircons and monazites from metamorphic rocks and migmatites suggests a metamorphic peak of the turbidite sequences at 1.87-1.88 Ga.

UR - http://www.scopus.com/inward/record.url?scp=3142674249&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:3142674249

VL - 395

SP - 311

EP - 314

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 3

ER -

ID: 93115681