| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5786926 | Russian Geology and Geophysics | 2017 | 13 Pages |
Abstract
volcanics are compared with subvolcanic granitoids of the Ognit complex in the Biryusa terrane (Sharyzhalgai basement inlier of the Siberian craton) adjacent to the Khamsara terrane. The volcanics and the granites are coeval and share compositional similarity. The Khamsara Formation is interpreted as a cap complex that marks the upper age bound of the accretionary-collisional events when amalgamated terranes in this part of the Central Asian orogen accreted to the Siberian craton.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
S.I. Shkol'nik, A.V. Ivanov, L.Z. Reznitsky, E.F. Letnikova, Hyaiyu He, Y. Zhiqlang, Youjueen Li, I.A. Vishnevskaya, I.G. Barash,