U–Pb SHRIMP II age and origin of zircon from lhertzolite of the bug Paleoarchean complex, Ukrainian Shield

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U–Pb SHRIMP II age and origin of zircon from lhertzolite of the bug Paleoarchean complex, Ukrainian Shield. / Lobach-Zhuchenko, S. B.; Baltybaev, Sh K.; Glebovitsky, V. A.; Sergeev, S. A.; Lokhov, K. O.; Egorova, Yu S.; Balagansky, V. V.; Skublov, S. G.; Galankina, O. L.; Stepanyuk, L. M.

In: Doklady Earth Sciences, Vol. 477, No. 2, 01.12.2017, p. 1391-1395.

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

Author

Lobach-Zhuchenko, S. B. ; Baltybaev, Sh K. ; Glebovitsky, V. A. ; Sergeev, S. A. ; Lokhov, K. O. ; Egorova, Yu S. ; Balagansky, V. V. ; Skublov, S. G. ; Galankina, O. L. ; Stepanyuk, L. M. / U–Pb SHRIMP II age and origin of zircon from lhertzolite of the bug Paleoarchean complex, Ukrainian Shield. In: Doklady Earth Sciences. 2017 ; Vol. 477, No. 2. pp. 1391-1395.

BibTeX

@article{4c1e988c87294a35a1963696d4fc5c4d,

title = "U–Pb SHRIMP II age and origin of zircon from lhertzolite of the bug Paleoarchean complex, Ukrainian Shield",

abstract = "Complex study of the U–Pb and Lu–Hf systems of zircon from a lhertzolite lens of Archean gneiss enderbites of the Bug complex, Ukrainian Shield, showed that ultramafic magma was contaminated by the material of the country gneiss enderbites. The age of the zircons of 2.81 ± 0.05 Ga corresponds to the period of ultramafic magmatism within the Bug complex. Previously, this peak of endogenic activity was considered the stage of manifestation of metamorphism and magmatism of mafic composition.",

author = "Lobach-Zhuchenko, {S. B.} and Baltybaev, {Sh K.} and Glebovitsky, {V. A.} and Sergeev, {S. A.} and Lokhov, {K. O.} and Egorova, {Yu S.} and Balagansky, {V. V.} and Skublov, {S. G.} and Galankina, {O. L.} and Stepanyuk, {L. M.}",

year = "2017",

month = dec,

day = "1",

doi = "10.1134/S1028334X17120157",

language = "English",

volume = "477",

pages = "1391--1395",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "2",

}

RIS

TY - JOUR

T1 - U–Pb SHRIMP II age and origin of zircon from lhertzolite of the bug Paleoarchean complex, Ukrainian Shield

AU - Lobach-Zhuchenko, S. B.

AU - Baltybaev, Sh K.

AU - Glebovitsky, V. A.

AU - Sergeev, S. A.

AU - Lokhov, K. O.

AU - Egorova, Yu S.

AU - Balagansky, V. V.

AU - Skublov, S. G.

AU - Galankina, O. L.

AU - Stepanyuk, L. M.

PY - 2017/12/1

Y1 - 2017/12/1

N2 - Complex study of the U–Pb and Lu–Hf systems of zircon from a lhertzolite lens of Archean gneiss enderbites of the Bug complex, Ukrainian Shield, showed that ultramafic magma was contaminated by the material of the country gneiss enderbites. The age of the zircons of 2.81 ± 0.05 Ga corresponds to the period of ultramafic magmatism within the Bug complex. Previously, this peak of endogenic activity was considered the stage of manifestation of metamorphism and magmatism of mafic composition.

AB - Complex study of the U–Pb and Lu–Hf systems of zircon from a lhertzolite lens of Archean gneiss enderbites of the Bug complex, Ukrainian Shield, showed that ultramafic magma was contaminated by the material of the country gneiss enderbites. The age of the zircons of 2.81 ± 0.05 Ga corresponds to the period of ultramafic magmatism within the Bug complex. Previously, this peak of endogenic activity was considered the stage of manifestation of metamorphism and magmatism of mafic composition.

UR - http://www.scopus.com/inward/record.url?scp=85039991782&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17120157

DO - 10.1134/S1028334X17120157

M3 - Article

AN - SCOPUS:85039991782

VL - 477

SP - 1391

EP - 1395

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 75533459