An Abnormal Isotopic Composition of Oxygen in Zircon from Corundum-Bearing Metasomatites of the Dyadina Gora Ore Occurrence, Belomorian Mobile Belt. / Skublov, S. G.; Bushmin, S. A.; Kuznetsov, A. B.; Li, X. H.; Li, Q. L.; Levashova, E. V.; Savva, E. V.
In: Doklady Earth Sciences, Vol. 491, No. 2, 01.04.2020, p. 247-252.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - An Abnormal Isotopic Composition of Oxygen in Zircon from Corundum-Bearing Metasomatites of the Dyadina Gora Ore Occurrence, Belomorian Mobile Belt
AU - Skublov, S. G.
AU - Bushmin, S. A.
AU - Kuznetsov, A. B.
AU - Li, X. H.
AU - Li, Q. L.
AU - Levashova, E. V.
AU - Savva, E. V.
N1 - Publisher Copyright: © 2020, Pleiades Publishing, Ltd. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/4/1
Y1 - 2020/4/1
N2 - Abstract: For the first time, the isotopic composition of oxygen, the content of trace elements, and the U–Pb zircon age were determined for kyanite–gedrite metasomatites from the Dyadina Gora ore occurrence, Belomorian Mobile Belt, Fennoscandian Shield. The zircon cores preserved from the protolith are characterized by a magmatic REE distribution and an average value of δ18O of about 3.0‰, and their age is close to 2400 Ma. The inner zones around the cores and rims of zircon were formed during metasomatic processes at the time of the Svecofennian metamorphism about 1870–1880 Ma ago, experienced strong fluid reworking, and are characterized by a decreased δ18O value to –0.9‰.
AB - Abstract: For the first time, the isotopic composition of oxygen, the content of trace elements, and the U–Pb zircon age were determined for kyanite–gedrite metasomatites from the Dyadina Gora ore occurrence, Belomorian Mobile Belt, Fennoscandian Shield. The zircon cores preserved from the protolith are characterized by a magmatic REE distribution and an average value of δ18O of about 3.0‰, and their age is close to 2400 Ma. The inner zones around the cores and rims of zircon were formed during metasomatic processes at the time of the Svecofennian metamorphism about 1870–1880 Ma ago, experienced strong fluid reworking, and are characterized by a decreased δ18O value to –0.9‰.
KW - Belomorian Mobile Belt
KW - Dyadina Gora ore occurrence
KW - oxygen isotope composition
KW - zircon
UR - http://www.scopus.com/inward/record.url?scp=85086385744&partnerID=8YFLogxK
U2 - 10.1134/S1028334X20040170
DO - 10.1134/S1028334X20040170
M3 - Article
AN - SCOPUS:85086385744
VL - 491
SP - 247
EP - 252
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -
ID: 75949940