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The oldest continental weathering profile formed after granites on the Baltic Shield. / Matrenichev, V. A.; Pin'kova, L. O.; Levchenkov, O. A.; Makeev, A. F.; Yakovleva, S. Z.; Alfimova, N. A.

In: Doklady Earth Sciences, Vol. 400, No. 1, 01.2005, p. 62-66.

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

Harvard

Matrenichev, VA, Pin'kova, LO, Levchenkov, OA, Makeev, AF, Yakovleva, SZ & Alfimova, NA 2005, 'The oldest continental weathering profile formed after granites on the Baltic Shield', Doklady Earth Sciences, vol. 400, no. 1, pp. 62-66.

APA

Matrenichev, V. A., Pin'kova, L. O., Levchenkov, O. A., Makeev, A. F., Yakovleva, S. Z., & Alfimova, N. A. (2005). The oldest continental weathering profile formed after granites on the Baltic Shield. Doklady Earth Sciences, 400(1), 62-66.

Vancouver

Matrenichev VA, Pin'kova LO, Levchenkov OA, Makeev AF, Yakovleva SZ, Alfimova NA. The oldest continental weathering profile formed after granites on the Baltic Shield. Doklady Earth Sciences. 2005 Jan;400(1):62-66.

Author

Matrenichev, V. A. ; Pin'kova, L. O. ; Levchenkov, O. A. ; Makeev, A. F. ; Yakovleva, S. Z. ; Alfimova, N. A. / The oldest continental weathering profile formed after granites on the Baltic Shield. In: Doklady Earth Sciences. 2005 ; Vol. 400, No. 1. pp. 62-66.

BibTeX

@article{1e016d9077a64cf591d4713313602727,
title = "The oldest continental weathering profile formed after granites on the Baltic Shield",
abstract = "The regional stratigraphic scheme of the Karelia-Kola region serves as the basis for the general Lower Precambrian scale of Russia. However, many problems associated with the Karelian stratigraphy are revised upon the appearance of new factual material. One of the most important, yet least developed problems of the Upper Archean (Lopian) stratigraphy is the relationship between supracrustal greenstone complexes and their basements. Usually, the Lopian basement and basal rocks lack reliably established relict structures of greenstone belts. Therefore, reconstructing the paleotectonic settings of the Archean volcanic belts' initial evolutionary stage is extremely complicated. The present work is devoted to describing the relationship between volcanic rocks and basement granitoids in the northeastern flank of the Lekhta structure, northern Karelia.",
author = "Matrenichev, {V. A.} and Pin'kova, {L. O.} and Levchenkov, {O. A.} and Makeev, {A. F.} and Yakovleva, {S. Z.} and Alfimova, {N. A.}",
year = "2005",
month = jan,
language = "English",
volume = "400",
pages = "62--66",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - The oldest continental weathering profile formed after granites on the Baltic Shield

AU - Matrenichev, V. A.

AU - Pin'kova, L. O.

AU - Levchenkov, O. A.

AU - Makeev, A. F.

AU - Yakovleva, S. Z.

AU - Alfimova, N. A.

PY - 2005/1

Y1 - 2005/1

N2 - The regional stratigraphic scheme of the Karelia-Kola region serves as the basis for the general Lower Precambrian scale of Russia. However, many problems associated with the Karelian stratigraphy are revised upon the appearance of new factual material. One of the most important, yet least developed problems of the Upper Archean (Lopian) stratigraphy is the relationship between supracrustal greenstone complexes and their basements. Usually, the Lopian basement and basal rocks lack reliably established relict structures of greenstone belts. Therefore, reconstructing the paleotectonic settings of the Archean volcanic belts' initial evolutionary stage is extremely complicated. The present work is devoted to describing the relationship between volcanic rocks and basement granitoids in the northeastern flank of the Lekhta structure, northern Karelia.

AB - The regional stratigraphic scheme of the Karelia-Kola region serves as the basis for the general Lower Precambrian scale of Russia. However, many problems associated with the Karelian stratigraphy are revised upon the appearance of new factual material. One of the most important, yet least developed problems of the Upper Archean (Lopian) stratigraphy is the relationship between supracrustal greenstone complexes and their basements. Usually, the Lopian basement and basal rocks lack reliably established relict structures of greenstone belts. Therefore, reconstructing the paleotectonic settings of the Archean volcanic belts' initial evolutionary stage is extremely complicated. The present work is devoted to describing the relationship between volcanic rocks and basement granitoids in the northeastern flank of the Lekhta structure, northern Karelia.

UR - http://www.scopus.com/inward/record.url?scp=16644386732&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:16644386732

VL - 400

SP - 62

EP - 66

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 9371474