Late Mesozoic rifting at the flanks of the Dzhagda segment of the Mongolia-Okhotsk collisional orogen: global and regional aspects
The role of rifting in the formation of the recent structure of the Mongolia-Okhotsk orogen is extremely high, but it is still underestimated with regard to flanks of the Dzhagda segment of this orogen. Current researches refer to a combination of physical and chemical processes in the depth of the...
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| Format: | Article |
| Language: | English |
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Institute of the Earth's crust, Siberian Branch of RAS
2017-03-01
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| Series: | Geodinamika i Tektonofizika |
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| Online Access: | https://www.gt-crust.ru/jour/article/view/337 |