| Autor: |
Logatchev, N.A., Zorin, Yu.A. |
| Zdroj: |
Tectonophysics; January 1992, Vol. 208 Issue: 1 p273-286, 14p |
| Abstrakt: |
The Cenozoic Baikal rift zone is superimposed on the Caledonian Baikal fold belt, representing the suture between the Precambrian Siberian craton and several microcontinents. The Baikal rift zone consists of a system of disconnected fault-bounded basins and extensional and wrench faults that straddles a major arch, having a topographic relief of 2–3 km. Rifting activity commenced during the Oligocène and is still active as evident from high seismicity of the Baikal rift zone. |
| Databáze: |
Supplemental Index |
| Externí odkaz: |
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