Nature and Age of Detrital Zircons from Rocks of the Shear Zone: The Problem of Occurrence of the Archean Basement in the Transangarian Yenisei Ridge
Petrogeochemical and geochronological study of boudined quartzite sandstones and tonalites, as well as host amphibolites, in the shear zone showed that potential sources of detrital zircons were Neoarchean–Paleoproterozoic rocks of the Angara–Kan block and products of their metamorphism. Interpretat...
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| Veröffentlicht in: | Doklady earth sciences 2018-05, Vol.480 (1), p.568-572 |
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| creator | Likhanov, I. I. Kozlov, P. S. Reverdatto, V. V. Popov, N. V. |
| description | Petrogeochemical and geochronological study of boudined quartzite sandstones and tonalites, as well as host amphibolites, in the shear zone showed that potential sources of detrital zircons were Neoarchean–Paleoproterozoic rocks of the Angara–Kan block and products of their metamorphism. Interpretation of the available data does not confirm the inferred presence of the Early Precambrian basement of the Siberian Craton in the Transangara region. |
| doi_str_mv | 10.1134/S1028334X18050161 |
| format | Article |
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| subjects | Amphibolites Cratons Earth and Environmental Science Earth Sciences Geochronology Geology Isotopes Metamorphic rocks Metamorphism Metamorphism (Geology) Precambrian Quartzite Radiometric dating Rock Rocks Sandstone Shear zone Zirconium |
| title | Nature and Age of Detrital Zircons from Rocks of the Shear Zone: The Problem of Occurrence of the Archean Basement in the Transangarian Yenisei Ridge |
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