|
ИСТИНА |
Войти в систему Регистрация |
ИПМех РАН |
||
Seismicity and fault plane solutions of intermediate depth earthquakes in the Pamirs-Hindu-Kush regionстатья
Информация о цитировании статьи получена из
Web of Science
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 16 января 2019 г.
- Авторы: Roecker S.W., Soboleva O.V., Nersesov I.L., Lukk A.A., D Hatzfeld D., Chatelain J.L., Molnar P.
- Журнал: Journal of Geophysical Research
- Том: 85
- Номер: 3
- Год издания: 1980
- Издательство: William Byrd Press for John Hopkins Press
- Местоположение издательства: United States
- Первая страница: 1358
- Последняя страница: 1364
- Аннотация: Abstract. Relocations of earthquakes, recorded by a local network of stations in Afghanistan and Tadjikistan in 1966 and 1967, indicate a narrow seismic zone (width • 30 kin) dipping steeply into the mantle to a depth of 300 km beneath the Pamir and Hindu Kush ranges. Very low seismicity was observed at depths less than about 70 kin, the approximate depth of the Moho. Clear gaps in activity exist also within the zone of intermediate depth seismicity. One gap, about 50 km wide near 37°N and at depths greater than 100 km, separates a steeply northward dipping zone to the southwest from a steeply southeastward dipping zone to the northeast. This gap probably marks either a tear in the downgoing slab or a gap between two oppositely dipping slabs. Fault plane solutions, determined by Soboleva for events between 1960 and 1967, generally show steeply plunging T axes approximately within the planar seismic zone. They therefore are grossly similar to those at island arcs where no deep earthquakes occur and presumably result from gravitational body forces acting on a relatively dense slab of lithosphere. At the same time there is a very large variation in the fault plane solutions, much larger than is common at island arcs.
- Добавил в систему: Лукк Альберт Артурович