Standard

The late Karelian in the stratigraphic scale of Russia : Determination of its lower boundary and regional units in the stratotype area. / Shul'diner, V. I.; Levchenkov, O. A.; Yakovleva, S. Z.; Makeev, A. F.; Komarov, A. N.; Konopel'ko, D. L.; Baltybaev, Sh K.; Kozyreva, I. V.

In: Stratigraphy and Geological Correlation, Vol. 8, No. 6, 01.11.2000, p. 544-556.

Research output: Contribution to journal › Article › peer-review

Harvard

Shul'diner, VI, Levchenkov, OA, Yakovleva, SZ, Makeev, AF, Komarov, AN, Konopel'ko, DL, Baltybaev, SK & Kozyreva, IV 2000, 'The late Karelian in the stratigraphic scale of Russia: Determination of its lower boundary and regional units in the stratotype area', Stratigraphy and Geological Correlation, vol. 8, no. 6, pp. 544-556.

APA

Shul'diner, V. I., Levchenkov, O. A., Yakovleva, S. Z., Makeev, A. F., Komarov, A. N., Konopel'ko, D. L., Baltybaev, S. K., & Kozyreva, I. V. (2000). The late Karelian in the stratigraphic scale of Russia: Determination of its lower boundary and regional units in the stratotype area. Stratigraphy and Geological Correlation, 8(6), 544-556.

Vancouver

Shul'diner VI, Levchenkov OA, Yakovleva SZ, Makeev AF, Komarov AN, Konopel'ko DL et al. The late Karelian in the stratigraphic scale of Russia: Determination of its lower boundary and regional units in the stratotype area. Stratigraphy and Geological Correlation. 2000 Nov 1;8(6):544-556.

Author

Shul'diner, V. I. ; Levchenkov, O. A. ; Yakovleva, S. Z. ; Makeev, A. F. ; Komarov, A. N. ; Konopel'ko, D. L. ; Baltybaev, Sh K. ; Kozyreva, I. V. / The late Karelian in the stratigraphic scale of Russia : Determination of its lower boundary and regional units in the stratotype area. In: Stratigraphy and Geological Correlation. 2000 ; Vol. 8, No. 6. pp. 544-556.

BibTeX

@article{d27e0bebc0d8451683a2a33a80d0a676,
title = "The late Karelian in the stratigraphic scale of Russia: Determination of its lower boundary and regional units in the stratotype area",
abstract = "The U-Pb zircon age is determined for stratigraphically important Upper Karelian structures of the northern Ladoga region. The age of the Sortavala Group volcanics is assumed to be 1.97-1.95 Ga that coincides with age of the Outokumpu and Jormua ophiolites in Finland. The Sortavala and coeval Suisar groups are recommended to be distinguish as the Livvian, the initial regional unit of the upper Karelian, which, along with ophiolites of Finland, marks the opening stage of the Svecofennian belt. The overlying Ladoga Group is a stratotype of the early Ladogian marking the mature evolutionary stage of Svecofennides. The upper boundary of the Ladoga Group is established on the basis of gabbroid intrusions intersecting the group and dated back to 1.88-1.89 Ga. The subsequent late Ladogian interval (up to 1.80 Ga) that characterizes an intense volcanism in the region is missing from the successions.",
keywords = "Isotope dating, Ladoga Group, Lower Proterozoic, Sortavala Group, Upper Karelian",
author = "Shul'diner, {V. I.} and Levchenkov, {O. A.} and Yakovleva, {S. Z.} and Makeev, {A. F.} and Komarov, {A. N.} and Konopel'ko, {D. L.} and Baltybaev, {Sh K.} and Kozyreva, {I. V.}",
year = "2000",
month = nov,
day = "1",
language = "English",
volume = "8",
pages = "544--556",
journal = "Stratigraphy and Geological Correlation",
issn = "0869-5938",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "6",

}

RIS

TY - JOUR

T1 - The late Karelian in the stratigraphic scale of Russia

T2 - Determination of its lower boundary and regional units in the stratotype area

AU - Shul'diner, V. I.

AU - Levchenkov, O. A.

AU - Yakovleva, S. Z.

AU - Makeev, A. F.

AU - Komarov, A. N.

AU - Konopel'ko, D. L.

AU - Baltybaev, Sh K.

AU - Kozyreva, I. V.

PY - 2000/11/1

Y1 - 2000/11/1

N2 - The U-Pb zircon age is determined for stratigraphically important Upper Karelian structures of the northern Ladoga region. The age of the Sortavala Group volcanics is assumed to be 1.97-1.95 Ga that coincides with age of the Outokumpu and Jormua ophiolites in Finland. The Sortavala and coeval Suisar groups are recommended to be distinguish as the Livvian, the initial regional unit of the upper Karelian, which, along with ophiolites of Finland, marks the opening stage of the Svecofennian belt. The overlying Ladoga Group is a stratotype of the early Ladogian marking the mature evolutionary stage of Svecofennides. The upper boundary of the Ladoga Group is established on the basis of gabbroid intrusions intersecting the group and dated back to 1.88-1.89 Ga. The subsequent late Ladogian interval (up to 1.80 Ga) that characterizes an intense volcanism in the region is missing from the successions.

AB - The U-Pb zircon age is determined for stratigraphically important Upper Karelian structures of the northern Ladoga region. The age of the Sortavala Group volcanics is assumed to be 1.97-1.95 Ga that coincides with age of the Outokumpu and Jormua ophiolites in Finland. The Sortavala and coeval Suisar groups are recommended to be distinguish as the Livvian, the initial regional unit of the upper Karelian, which, along with ophiolites of Finland, marks the opening stage of the Svecofennian belt. The overlying Ladoga Group is a stratotype of the early Ladogian marking the mature evolutionary stage of Svecofennides. The upper boundary of the Ladoga Group is established on the basis of gabbroid intrusions intersecting the group and dated back to 1.88-1.89 Ga. The subsequent late Ladogian interval (up to 1.80 Ga) that characterizes an intense volcanism in the region is missing from the successions.

KW - Isotope dating

KW - Ladoga Group

KW - Lower Proterozoic

KW - Sortavala Group

KW - Upper Karelian

UR - http://www.scopus.com/inward/record.url?scp=4544330704&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:4544330704

VL - 8

SP - 544

EP - 556

JO - Stratigraphy and Geological Correlation

JF - Stratigraphy and Geological Correlation

SN - 0869-5938

IS - 6

ER -

ID: 41124403