Cambrian/Ordovician boundary as a milestone in the sedimentation history of the southern Siberian craton: Evidence from U-Pb dating of detrital zircons
•The Upper Lena Fm. is part of Late Cambrian sedimentary cover of the Siberian craton.•The ages of detrital zircons are mostly Early Paleozoic.•Early Precambrian and Neoproterozoic detrital zircons are subordinate.•The Upper Lena deposition is a key milestone in the geological history of Siberia. Th...
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Published in | Journal of Asian Earth Sciences: X Vol. 8; p. 100107 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.12.2022
Elsevier |
Subjects | |
Online Access | Get full text |
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