| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8908370 | Journal of Geodynamics | 2018 | 66 Pages |
Abstract
The warm-water Bashkirian-Asselian biota suggests that the Mendeleev-Chukotka-Wrangel block was a low-latitude shallow basin with predominant carbonate sedimentation, being part of the Arctida supercontinent, connected temporarily with the eastern margin of Laurasia (Chukcha-Alaska block).
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
O.L. Kossovaya, T.Yu. Tolmacheva, O.V. Petrov, T.N. Isakova, R.M. Ivanova, E.S. Mirolyubova, P.V. Rekant, E.A. Gusev,