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Dating of high-aluminous metamorphic paragenesis in the potassium zone of the Ladoga region (Baltic shield). / Baltybaev, Sh K.; Levchenkov, O. A.; Glebovskij, V. A.; Levskij, L. K.; Makeev, A. F.; Ro, N. I.

в: Doklady Akademii Nauk, Том 393, № 6, 2003, стр. 793-796.

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

Harvard

Baltybaev, SK, Levchenkov, OA, Glebovskij, VA, Levskij, LK, Makeev, AF & Ro, NI 2003, 'Dating of high-aluminous metamorphic paragenesis in the potassium zone of the Ladoga region (Baltic shield)', Doklady Akademii Nauk, Том. 393, № 6, стр. 793-796.

APA

Baltybaev, S. K., Levchenkov, O. A., Glebovskij, V. A., Levskij, L. K., Makeev, A. F., & Ro, N. I. (2003). Dating of high-aluminous metamorphic paragenesis in the potassium zone of the Ladoga region (Baltic shield). Doklady Akademii Nauk, 393(6), 793-796.

Vancouver

Baltybaev SK, Levchenkov OA, Glebovskij VA, Levskij LK, Makeev AF, Ro NI. Dating of high-aluminous metamorphic paragenesis in the potassium zone of the Ladoga region (Baltic shield). Doklady Akademii Nauk. 2003;393(6):793-796.

Author

Baltybaev, Sh K. ; Levchenkov, O. A. ; Glebovskij, V. A. ; Levskij, L. K. ; Makeev, A. F. ; Ro, N. I. / Dating of high-aluminous metamorphic paragenesis in the potassium zone of the Ladoga region (Baltic shield). в: Doklady Akademii Nauk. 2003 ; Том 393, № 6. стр. 793-796.

BibTeX

@article{471577a81edb48f78ee3ba285d00c94a,
title = "Dating of high-aluminous metamorphic paragenesis in the potassium zone of the Ladoga region (Baltic shield)",
abstract = "Dating of metamorphic processes is difficult due to genetic heterogeneity of metamorphic rock. Problem of dating is often connected with long and multistage proceeding of metamorphism. Time of process is determined by indirect method. This is not reliable approach. Time of metamorphism should directly be determined with the use of minerals, metamorphic origin of which is clear. Pb-Pb-investigation of metamorphogenic mineral, sillimanite have been performed. Results of the investigations have been presented. Method of step-by-step dissolution has been applied. Isotope investigation makes it possible to determine the time of peak of metamorphism.",
author = "Baltybaev, {Sh K.} and Levchenkov, {O. A.} and Glebovskij, {V. A.} and Levskij, {L. K.} and Makeev, {A. F.} and Ro, {N. I.}",
year = "2003",
language = "English",
volume = "393",
pages = "793--796",
journal = "ДОКЛАДЫ АКАДЕМИИ НАУК",
issn = "0869-5652",
publisher = "Издательство {"}Наука{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Dating of high-aluminous metamorphic paragenesis in the potassium zone of the Ladoga region (Baltic shield)

AU - Baltybaev, Sh K.

AU - Levchenkov, O. A.

AU - Glebovskij, V. A.

AU - Levskij, L. K.

AU - Makeev, A. F.

AU - Ro, N. I.

PY - 2003

Y1 - 2003

N2 - Dating of metamorphic processes is difficult due to genetic heterogeneity of metamorphic rock. Problem of dating is often connected with long and multistage proceeding of metamorphism. Time of process is determined by indirect method. This is not reliable approach. Time of metamorphism should directly be determined with the use of minerals, metamorphic origin of which is clear. Pb-Pb-investigation of metamorphogenic mineral, sillimanite have been performed. Results of the investigations have been presented. Method of step-by-step dissolution has been applied. Isotope investigation makes it possible to determine the time of peak of metamorphism.

AB - Dating of metamorphic processes is difficult due to genetic heterogeneity of metamorphic rock. Problem of dating is often connected with long and multistage proceeding of metamorphism. Time of process is determined by indirect method. This is not reliable approach. Time of metamorphism should directly be determined with the use of minerals, metamorphic origin of which is clear. Pb-Pb-investigation of metamorphogenic mineral, sillimanite have been performed. Results of the investigations have been presented. Method of step-by-step dissolution has been applied. Isotope investigation makes it possible to determine the time of peak of metamorphism.

UR - http://www.scopus.com/inward/record.url?scp=4544319008&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:4544319008

VL - 393

SP - 793

EP - 796

JO - ДОКЛАДЫ АКАДЕМИИ НАУК

JF - ДОКЛАДЫ АКАДЕМИИ НАУК

SN - 0869-5652

IS - 6

ER -

ID: 93116013