INTERNAL STRUCTURES OF FAULT ZONES IN THE PRIOLKHONIE AND EVOLUTION OF THE STATE OF STRESSES OF THE UPPER CRUST OF THE BAIKAL RIFT
The Priolkhonie is a tectonic block located in the central part of the Baikalsky Ridge; it was shifted in the Cenozoic, yet remains above the water level of Lake Baikal. In view of its unique positioning and abundant rock outcropped sites, especially at shorelines, we conducted studies of internal s...
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
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Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2015-09-01
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| Saila: | Геодинамика и тектонофизика |
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| Sarrera elektronikoa: | https://www.gt-crust.ru/jour/article/view/112 |
| Etiketak: |
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