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| Content Provider | Springer Nature Link |
|---|---|
| Author | Letnikova, E. F. Izokh, A. E. Nikolenko, E. I. Pokhilenko, N. P. Shelestov, V. O. Hilen, Geng Lobav, S. S. |
| Copyright Year | 2014 |
| Abstract | The U-Pb (LA-ICP-MS) age was determined for detrital zircons from the Upper Triassic volcanomictic rocks of the Osipai Formation (Bulkur River) of the northeastern Siberian Platform. The mineral composition and textural and structural peculiarities of these rocks indicate their formation as a result of eruptive high-potassium trachitic volcanism 235 Ma ago. More local manifestation of this volcanism in the area of the Lena River is evident from the U-Pb age of detrital zircons from the area of the Khatystakh River, which were previously ascribed to the Carnian Stage. Our data indicate redeposition of the clastic material of the Carnian diamond horizon in the post-Jurassic period. |
| Starting Page | 1344 |
| Ending Page | 1347 |
| Page Count | 4 |
| File Format | |
| ISSN | 1028334X |
| Journal | Doklady Earth Sciences |
| Volume Number | 459 |
| Issue Number | 1 |
| e-ISSN | 15318354 |
| Language | English |
| Publisher | Pleiades Publishing |
| Publisher Date | 2014-12-06 |
| Publisher Place | Moscow |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Earth Sciences |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences |
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