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 inJournal of Asian Earth Sciences: X Vol. 8; p. 100107
Main Authors Gladkochub, Dmitrii P., Motova, Zinaida L., Donskaya, Tatiana V., Khubanov, Valentin B., Sizov, Alexander V.
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.12.2022
Elsevier
Subjects
Clastic sediments
Detrital zircons
Late Cambrian
Sedimentary cover
Siberian craton
U-Pb age
Detrital zircons
Late Cambrian
Sedimentary cover
U-Pb age
Clastic sediments
Siberian craton
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Abstract •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. The paper presents petrographic, geochemical, and new U-Pb zircon (LA-ICP-MS) geochronological data on the Upper Lena Fm. sediments which make part of the Cambrian sedimentary cover of the Siberian craton. The composition of lithic fragments in these clastic sediments, including mafic and felsic volcanics and granitoids, along with the correlation of major element ratios and the values of trace-element ratios point to predominant igneous (mainly felsic) rocks in the provenance. The U-Pb ages of detrital zircons from the sampled Upper Lena Fm. sandstones are mostly Early Paleozoic (∼500 Ma), with very few Archean-Paleoproterozoic determinations and quite many Neoproterozoic zircons. Ediacaran and Earliest Cambrian clastic sediments bearing Early Precambrian and Neoproterozoic detrital zircons, as well as Neoproterozoic and Early Paleozoic complexes of the Central Asian Orogenic Belt, could provide material for the Upper Lena clastic deposition. The geochronological evidence shows that the Upper Lena Fm. sandstones were deposited over vast territories of the southern Siberian craton in the Late Cambrian, in a single sedimentary basin, and originated from the same provenance. The Upper Lena deposition event in the Late Cambrian, immediately before the Ordovician period, makes a key milestone in the geological history of Siberia: the end of a large-scale Early Cambrian transgression and the beginning of gradual uplift of the southern craton margin, at least till the Carboniferous, which was associated with the formation of the Central Asian Orogenic Belt, a major tectonic unit of Asia.
AbstractList The paper presents petrographic, geochemical, and new U-Pb zircon (LA-ICP-MS) geochronological data on the Upper Lena Fm. sediments which make part of the Cambrian sedimentary cover of the Siberian craton. The composition of lithic fragments in these clastic sediments, including mafic and felsic volcanics and granitoids, along with the correlation of major element ratios and the values of trace-element ratios point to predominant igneous (mainly felsic) rocks in the provenance. The U-Pb ages of detrital zircons from the sampled Upper Lena Fm. sandstones are mostly Early Paleozoic (∼500 Ma), with very few Archean-Paleoproterozoic determinations and quite many Neoproterozoic zircons. Ediacaran and Earliest Cambrian clastic sediments bearing Early Precambrian and Neoproterozoic detrital zircons, as well as Neoproterozoic and Early Paleozoic complexes of the Central Asian Orogenic Belt, could provide material for the Upper Lena clastic deposition. The geochronological evidence shows that the Upper Lena Fm. sandstones were deposited over vast territories of the southern Siberian craton in the Late Cambrian, in a single sedimentary basin, and originated from the same provenance. The Upper Lena deposition event in the Late Cambrian, immediately before the Ordovician period, makes a key milestone in the geological history of Siberia: the end of a large-scale Early Cambrian transgression and the beginning of gradual uplift of the southern craton margin, at least till the Carboniferous, which was associated with the formation of the Central Asian Orogenic Belt, a major tectonic unit of Asia.
•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. The paper presents petrographic, geochemical, and new U-Pb zircon (LA-ICP-MS) geochronological data on the Upper Lena Fm. sediments which make part of the Cambrian sedimentary cover of the Siberian craton. The composition of lithic fragments in these clastic sediments, including mafic and felsic volcanics and granitoids, along with the correlation of major element ratios and the values of trace-element ratios point to predominant igneous (mainly felsic) rocks in the provenance. The U-Pb ages of detrital zircons from the sampled Upper Lena Fm. sandstones are mostly Early Paleozoic (∼500 Ma), with very few Archean-Paleoproterozoic determinations and quite many Neoproterozoic zircons. Ediacaran and Earliest Cambrian clastic sediments bearing Early Precambrian and Neoproterozoic detrital zircons, as well as Neoproterozoic and Early Paleozoic complexes of the Central Asian Orogenic Belt, could provide material for the Upper Lena clastic deposition. The geochronological evidence shows that the Upper Lena Fm. sandstones were deposited over vast territories of the southern Siberian craton in the Late Cambrian, in a single sedimentary basin, and originated from the same provenance. The Upper Lena deposition event in the Late Cambrian, immediately before the Ordovician period, makes a key milestone in the geological history of Siberia: the end of a large-scale Early Cambrian transgression and the beginning of gradual uplift of the southern craton margin, at least till the Carboniferous, which was associated with the formation of the Central Asian Orogenic Belt, a major tectonic unit of Asia.
ArticleNumber 100107
Author Gladkochub, Dmitrii P.
Motova, Zinaida L.
Khubanov, Valentin B.
Donskaya, Tatiana V.
Sizov, Alexander V.
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Keywords Detrital zircons
Late Cambrian
Sedimentary cover
U-Pb age
Clastic sediments
Siberian craton
Language English
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Snippet •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...
The paper presents petrographic, geochemical, and new U-Pb zircon (LA-ICP-MS) geochronological data on the Upper Lena Fm. sediments which make part of the...
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StartPage 100107
SubjectTerms Clastic sediments
Detrital zircons
Late Cambrian
Sedimentary cover
Siberian craton
U-Pb age
Title Cambrian/Ordovician boundary as a milestone in the sedimentation history of the southern Siberian craton: Evidence from U-Pb dating of detrital zircons
URI https://dx.doi.org/10.1016/j.jaesx.2022.100107
https://doaj.org/article/7e54ea2813fa4d7a9e759f6c5db00f90
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