POSSIBLE NATURE OF THE SEISMIC BOUNDARY AT A DEPTH OF 70 KM
| dc.contributor.author | Levin B.W. | |
| dc.contributor.author | Rodkin M.V. | |
| dc.contributor.author | Sasorova E.V. | |
| dc.date.accessioned | 2026-04-25T09:33:02Z | |
| dc.date.issued | 2007 | |
| dc.description.abstract | Classical works on seismology and the physics of the Earth distinguish a boundary at a depth of 70 km, which divides shallow-focus (shallow) and intermediate earthquakes that occupy the depth range from 70 to 300 km. It should be noted that shallow (<70 km) earthquakes comprise approximately 85% of the total number of recorded events. The nature of this boundary remains debatable so far. | |
| dc.identifier | https://elibrary.ru/item.asp?id=15292277 | |
| dc.identifier.citation | Doklady Earth Sciences, 2007, 414, 1, 578-581 | |
| dc.identifier.doi | 10.1134/S1028334X07040204 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/52634 | |
| dc.title | POSSIBLE NATURE OF THE SEISMIC BOUNDARY AT A DEPTH OF 70 KM | |
| dc.type | Статья |
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