FORMATION OF DIKES AND SILLS UNDER KLYUCHEVSKOI VOLCANO BY MAGMA INTRUSION THROUGH THE CONDUIT
| dc.contributor.author | Efimov A.B. | |
| dc.contributor.author | Ershova T.Ya. | |
| dc.contributor.author | Fedotov S.A. | |
| dc.date.accessioned | 2020-12-01T08:48:30Z | |
| dc.date.available | 2020-12-01T08:48:30Z | |
| dc.date.issued | 1996 | |
| dc.description.abstract | The problem of magma intrusion through conduit walls is examined using the example of Klyuchevskoi Volcano. Magma intrusion takes place at all depths; the initial break through the wallrocks occurs mainly as a vertical dike. The properties and behavior of the dike-invaded viscoelastic wallrocks are discussed. | |
| dc.identifier | https://elibrary.ru/item.asp?id=20957482 | |
| dc.identifier.citation | Volcanology & Seismology, 1996, , 1, 1-23 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/20044 | |
| dc.title | FORMATION OF DIKES AND SILLS UNDER KLYUCHEVSKOI VOLCANO BY MAGMA INTRUSION THROUGH THE CONDUIT | |
| dc.type | Статья |