Research output: Contribution to journal › Article › peer-review
New U–Pb isotopic data for detrital zircons from metasedimentary sequences of northwestern Taimyr. / Ershova, V. B.; Prokopiev, A. V.; Khudoley, A. K.; Proskurnin, V. F.; Andersen, T.; Kullerud, K.; Stepunina, M. A.; Kolchanov, D. A.
In: Doklady Earth Sciences, Vol. 474, No. 2, 01.06.2017, p. 613-616.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - New U–Pb isotopic data for detrital zircons from metasedimentary sequences of northwestern Taimyr
AU - Ershova, V. B.
AU - Prokopiev, A. V.
AU - Khudoley, A. K.
AU - Proskurnin, V. F.
AU - Andersen, T.
AU - Kullerud, K.
AU - Stepunina, M. A.
AU - Kolchanov, D. A.
PY - 2017/6/1
Y1 - 2017/6/1
N2 - This work presents the U–Pb (LA–ICP–MS) data of detrital zircons from metasedimentary sequences of northwestern Taimyr. An analysis of the youngest populations of detrital zircons testifies to the wide distribution of Cambrian sequences in the study area, but not Precambrian sequences as was considered earlier, and the need for a substantial revision of the stratigraphic scheme of this area. The detrital zircon age distribution shows that the Timan margin of the Baltic paleocontinent was a major provenance area of the Cambrian sediments in northern and northwestern Taimyr, as well as the coeval sediments of the Severnaya Zemlya archipelago.
AB - This work presents the U–Pb (LA–ICP–MS) data of detrital zircons from metasedimentary sequences of northwestern Taimyr. An analysis of the youngest populations of detrital zircons testifies to the wide distribution of Cambrian sequences in the study area, but not Precambrian sequences as was considered earlier, and the need for a substantial revision of the stratigraphic scheme of this area. The detrital zircon age distribution shows that the Timan margin of the Baltic paleocontinent was a major provenance area of the Cambrian sediments in northern and northwestern Taimyr, as well as the coeval sediments of the Severnaya Zemlya archipelago.
UR - http://www.scopus.com/inward/record.url?scp=85024101767&partnerID=8YFLogxK
U2 - 10.1134/S1028334X17060022
DO - 10.1134/S1028334X17060022
M3 - Article
AN - SCOPUS:85024101767
VL - 474
SP - 613
EP - 616
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -
ID: 36001401