Sources and Provenances of Late Cenozoic Sand Deposits of the Ol’khon Island (Baikal Rift Zone)
Geochronological (LA–ICP–MS) U–Th–Pb studies of detrital zircon of the Late Cenozoic sand deposits on Ol’khon Island have been performed. It has been shown that their main source is represented by Early Paleozoic igneous and metamorphic complexes of the Ol’khon Terrane of the Central-Asian Mobile be...
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| Veröffentlicht in: | Doklady earth sciences 2019, Vol.484 (1), p.45-47 |
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| creator | Kotov, A. B. Skovitina, T. M. Kovach, V. P. Sklyarov, E. V. Donskaya, T. V. Lopatin, D. V. Plotkina, Yu. V. Tolmacheva, E. V. Gorokhovskii, B. M. Buchnev, I. N. |
| description | Geochronological (LA–ICP–MS) U–Th–Pb studies of detrital zircon of the Late Cenozoic sand deposits on Ol’khon Island have been performed. It has been shown that their main source is represented by Early Paleozoic igneous and metamorphic complexes of the Ol’khon Terrane of the Central-Asian Mobile belt and Late Carboniferous–Early Permian granitoids of the Angara–Vitim batholite. Sands from the source were transported over a distance of no less than 100 km. It is supposed that it was effectuated by strong air flows, over the ice on the Lake Baikal in particular. |
| doi_str_mv | 10.1134/S1028334X19010203 |
| format | Article |
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It is supposed that it was effectuated by strong air flows, over the ice on the Lake Baikal in particular.</description><subject>Air flow</subject><subject>Carboniferous</subject><subject>Cenozoic</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochronology</subject><subject>Geological time</subject><subject>Geology</subject><subject>Granite</subject><subject>Lake ice</subject><subject>Lakes</subject><subject>Paleozoic</subject><subject>Permian</subject><subject>Phanerozoic Eon</subject><subject>Rift zones</subject><subject>Sand</subject><subject>Zircon</subject><subject>Zirconium</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1kM1KAzEUhQdRsFYfwF3AjS6m5r-ZZa1_hULFKoibIZ1J2rRjUpOpoCtfw9fzScw4gguRLHKTc76bm5Mkhwj2ECL0dIogFoTQB5TBWEKylXQQIygVhNHtWEc5bfTdZC-EJYSUUpZ1Ejl1G1-oAKQtwY13L8pK25ydBmNZKzBU1r05U4Bp4zhXaxdM_S3XCwUm1ef7x2rhLBiFqjEcn0mzkhW4NboGj86qk_1kR8sqqIOfvZvcX17cDa_T8eRqNByMU0n6ok5nVEPBMo4kwVyyEhUln7E-UoJIKsuS86Ik_SLTRHAkIOczNcswplgiCDNOSTc5avuuvXveqFDny_g1G5_MMSaUMcQwi65e65rLSuXGald7WcRVqidTxHm1ifcDJlDMhxMYAdQChXcheKXztTdP0r_mCOZN9Pmf6CODWyZEr50r_zvK_9AXamKEFA</recordid><startdate>2019</startdate><enddate>2019</enddate><creator>Kotov, A. 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N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Sources and Provenances of Late Cenozoic Sand Deposits of the Ol’khon Island (Baikal Rift Zone)</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2019</date><risdate>2019</risdate><volume>484</volume><issue>1</issue><spage>45</spage><epage>47</epage><pages>45-47</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>Geochronological (LA–ICP–MS) U–Th–Pb studies of detrital zircon of the Late Cenozoic sand deposits on Ol’khon Island have been performed. It has been shown that their main source is represented by Early Paleozoic igneous and metamorphic complexes of the Ol’khon Terrane of the Central-Asian Mobile belt and Late Carboniferous–Early Permian granitoids of the Angara–Vitim batholite. Sands from the source were transported over a distance of no less than 100 km. 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| subjects | Air flow Carboniferous Cenozoic Earth and Environmental Science Earth Sciences Geochronology Geological time Geology Granite Lake ice Lakes Paleozoic Permian Phanerozoic Eon Rift zones Sand Zircon Zirconium |
| title | Sources and Provenances of Late Cenozoic Sand Deposits of the Ol’khon Island (Baikal Rift Zone) |
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